WEBVTT

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 Recording. This is Paul, her and Jennifer Sweeney of Arizona State

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University interviewing Richard Valdez
at the SWC A offices in Salt Lake

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City on March 4th 2020. Rich. Thanks
for uh interviewing with us today.

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Thank you for asking me. Would you
just start out by telling us um, the

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positions that you've held in the
Adaptive Management Program over the

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years and the years that you were
participating? Yeah. Thank you. I um I

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started working um in the Grand Canyon
with Glen Canyon Dam operations and

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in 1989 that was when it was the Glen
Canyon environmental studies. G ce S

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under Dave Wagner and the Bureau of
Reclamation. And uh at that time, I

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was contracted to do a life history
and ecology of the Humpback job

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through the Grand Canyon. So that was
my first time there. And as a result

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of that involvement, I also did some
other things. I worked some with the

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wallaby tribe. So we extended a lot of
our investigations below Diamond

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Creek all the way to Pearce ferry. So
we were doing about 275 280 miles of

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the river that we were surveying for
fish populations. And with that, uh I

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, I then was asked to convene several
panels of scientists, one in 1999 to

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look at the possibility of a second
population of Humpback chub in the

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Grand Canyon. And I met with
geneticists and biologists to look at ideas

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of how to start Humpback job in the
Grand Canyon. That was about 1999.

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In 2000, I was involved in the low
steady summer flow experiment. I did

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the fisheries evaluation of that
experiment. And then in um in 2003, I was

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part of a team of scientists that were
looking at the possibility of a

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temperature control device for Glen
Canyon Dam. And that was being co

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ordinated by the Bureau of
Reclamation.

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And in 2004, I co ordinated a survey
of some of the tributaries in the

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Grand Canyon with Steve Carruthers. So
we looked not only at the main stem

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but also fisheries populations in
places like Shinan or Bright Angel Creek

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or Havasu Creek and some of the others
in the system. And then in, in 2010

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, I was asked by the,

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the Bureau of reclamation to convene a
science panel on reintroducing

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razorback sucker into the Grand
Canyon. And uh and then in, in 2012, I was

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asked to convene another science panel
by the seven Colorado River Basin

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States to evaluate possible
alternatives that would become part of the

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2016 temp eis temp was of course the
long term experimental management

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program for the Glen Canyon Dam. And
then, and then most recently, uh, I

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was, uh, asked to be a member of the
Brown Trout management team, looking

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at options of how to manage brown
trout, worked with, uh, Mike runs and

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Charles Yule to look at the options of
how to manage brown trout and

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reduce predation by brown trout on,
uh, on Humpback chub and on other

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trout species in the system,
especially in the tail water. So it's pretty

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much banned from about 1989 to here.
Most recently, 2019. It's a nice long

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tenure. Um, how much of the work that
you did was, uh, say contract

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research work with SWC A versus work,
um, directly as a participant in the

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Glen Canny Dam Adaptive Management
Program, like with AM Wig or Twig, can

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you? Yeah, most of it was contract
work. Most of it was contract work

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either either through Biow West or
through SWC A. And the Biow West work

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was that initial study of fisheries,
the life history ecology of Humpback

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job through the, through the canyon.
And then the subsequent to that, it's

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been through Biow West and I was
involved in a number of Am Wig and Twig

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meetings, but pretty much always as a,
as a linkage to one of these two

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companies, correct? So let's drill
down a bit on, um, the role of the

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Humpback Chub in the Adaptive
Management program, you're probably gonna be

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the most knowledgeable expert we
interview on the life history and the

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status and the recovery efforts of the
Humpback Chub. So, talk a little

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bit about how that all got started and
developed over time. Yeah, it, it,

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it's an important part of, uh, of the
Glen Canyon Dam operations because

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the Humpback Chub is perhaps one of
the keystone species, if not the

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keystone species for, for that
particular project in that operation. Um

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I've been uh the, the recovery team
leader for the Humpback Chub recovery

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team since 2015. So it's put me close
to some of the populations, not only

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in the Grand Canyon but in the upper
basin as well. But the interesting

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part about it is the, the genesis of
how the Humpback chub came into the

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important and significance that it
holds in the Grand Canyon. I started

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working in the upper Colorado River
basin in 1968 with a fellow graduate

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student, he was doing work on the
Colorado and Green Rivers and I was

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doing work in Alaska. So we would
trade trade off helping each other. And

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uh after that, then I was um uh I got
involved in some of the work earlier

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research. Now, this is before the
endangered Species Act was passed in

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1973. And at that time, um the
Humpback chub and the, what was at that

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time known as the Colorado squaw fish.
It is now called the Colorado pike

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minnow. At that time, those species
were included under the Endangered

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Species Conservation Act, the
Preservation Act of 66 and then the

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Conservation Act of 69 prior to the
passage of ES A. So, uh in 1973 when

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uh the endangered species act was, was
enacted and signed by President

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Nixon, those species then became part
of this suite of, of species in this

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country that people had to protect
somehow but no one, no one knew exactly

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how to do it. And so I was in on some
of the original uh environmental

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impact statements, the eas that
affected some of these species uh that,

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that, that took place in the uh
especially in the upper Colorado River

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basin. But it's interesting to note
that that in um and I was with fish

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and wildlife service starting in 1979

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I was hired by the service to start a
field station in Grand Junction,

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Colorado to do that specifically to
evaluate the distribution and

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abundance of these fish in the upper
Colorado river basin. So above Lake

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Powell, basically and in and in and
until 1980 from the time that the act

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was, was passed in 73 we had these
biological opinions that all declared

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jeopardy. In other words, that the
action would, would likely continue to

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jeopardy or continue to jeopardize the
existence of the species. Um in

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1980 with the, with the amendments to
the endangered species Act, that a

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concept of reasonable and prudent
alternatives was then put into the act

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which really opened the door and
allowed agencies now to start doing good

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things for the species to offset or
mitigate those potential bad things.

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And that, that became the heart of
what became then the Glen Canyon Dam

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eis is basically those reasonable and
prudent alternatives that were put

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forward. Now, the first E I was done,
of course, in 1995 when the Humpback

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job was, was listed and the biological
opinion was under a jeopardy

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determination. In other words, it was
declared that the operation of Glen

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Canyon Dam was likely to jeopardize
the continued existence of the species

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that changed in 2008

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when the service came up with a non
jeopardy determination and decided

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that instead they would go with
conservation measures which were finalized

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in 2010. So now we have an agency or
agencies, the Bureau of Reclamation

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and the Park Service in that case that
we're looking at ways to do things

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better as a way to benefit, not just
to mitigate the potential jeopardy

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effects, but also to benefit the
species. So, so the Humpback chub

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underwent uh a whole, I think
evolution of understanding of how that

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species worked out with the endangered
species Act, how they act was going

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to apply to that species specifically.
And the Grand Canyon became kind of

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the the stage for that to all take
place where the Grand Canyon supported

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the largest population of Humpback
chub known in the basin. There were six

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other populations in the upper basin,
but they were all smaller. But the

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Humpback job was the main driver. I
think of a lot of the actions that

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took place in that system and actions
in terms of modifying dam operations

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or actions, in terms of improving
habitat or reducing predation, all of

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those things, it was all of those
things. And initially, as a, as a fish

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biologist, my first reaction to seeing
a uh a large dam put in the middle

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of a river that used to be occupied by
these, these fish was that of

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course, that dam, first of all backed
up Lake Powell for about 200 miles

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and that meant there was 200 miles of
river that were under a lake. So it

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eliminated that habitat to the
species. And these are not lake dwellers

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except for the Razorback sucker. Uh
the Humpback chub and the pike minnow

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don't do well in lakes or reservoirs.
So that eliminated that habitat. But

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also what the dam did is it was now
drawing water from the, from the

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depths of the reservoir. What is known
as the Hypo Limn and that's the

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coal region. So you had coal releases
going downstream that we all knew

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was not good for the warm water native
fish like Humpback chop. So our

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first reaction was to and then I I
talk II I say that collectively for

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most fish biologists was to say we're
going to somehow need to offset that

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cold water coming out of the dam by
some kind of temperature control

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devices. So the T CD became a pretty
important and controversial. I might

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say uh proposal starting in about 2002
or 2003 where some of us were

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advocating to have the dam modified to
allow warmer water, warmer, more

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surface water to be released and warm
the water downstream. For the

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Humpback chub.

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In retrospect, as it turns out, that
probably was

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a lack or a not a good enough
understanding by the biologist to really

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know what was going on. As it turns
out, it could be, it could very well

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be that the coal releases have been
part of the savings grace for the

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Humpback job in Grand Canyon. So in
that those coal releases now prevent

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or at least inhibit other non native
warm water fish that are predators or

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competitors to the Humpback job from
entering and coming into the system.

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And in addition to that, the Humpback
chub in the Grand Canyon has been

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using the little Colorado River which
is a seasonally warm system for

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spawning. So it made and and still
does. It makes for an ideal situation

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for that fish to be able to live as
adults in the main stem and then

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migrate annually into the little
Colorado River and spawn in warmer water.

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And then they're young, then descend
down into the main stem. So that's

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the way, that's the way the situation
is today. And, and we didn't know

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that. Of course, at that time, many of
us were advocating to have a

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temperature control device. And in
fact, uh we had a series of meetings

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with the bureau of reclamation and
many scientists and in fact,

00:13:35.149 --> 00:13:41.395
reclamation even did a, a rough
estimate of what it would cost to put in a

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a uh uh a select what's known as a
selective withdrawal temperature

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control device, which would mean that
that the uh the gates at the pen

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stocks where the water leaves the
reservoir and goes through the dam, the

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gates would be modified with elevators
so that they would, you'd have the

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op the option of basically withdrawing
water from any level that you want

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within a given range. So you could mix
it warm with cold and get target

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temperatures. The only problem was
that the estimated price tag was about

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$100 million

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and that of course, raised many
eyebrows and caused much concern as to how

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serious we really wanted to get about
that proposal. Mhm.

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So um

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so one of the lessons we learned, I
think as scientists in, in going

00:14:43.178 --> 00:14:48.167
through Glen Canyon Dam and evaluating
the effects and sitting to sitting

00:14:48.200 --> 00:14:52.326
down together and coming up with
different alternatives was that in the

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end, uh it's Mother Nature that really
drives everything. And as we were

00:14:59.788 --> 00:15:04.336
considering a temperature control
device, of course, the elevations of

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both Lake Powell and Lake Mead were
dropping and with a decline in

00:15:09.489 --> 00:15:17.196
elevation of uh of Lake Powell, we now
started to see warm water being

00:15:17.229 --> 00:15:23.895
released from the reservoir by warm. I
mean, what had been 10 °C 8 to 10

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°C releases were now 1213, 14, maybe
even up to 15 or 16 °C. But that,

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that warm water was coming out in
October and November in the fall. And

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the reason for that is that um in the
fall, the reservoir overturns there

00:15:43.469 --> 00:15:47.677
is what is known as a fall overturn
and as that warmer surface water is

00:15:47.710 --> 00:15:54.917
mixing with a lower water, it comes in
contact with the those pen stocks

00:15:54.950 --> 00:15:59.047
where water is being withdrawn through
the dam. And so that's why we see

00:15:59.080 --> 00:16:04.375
that warmer water at that time. Well,
it just so happens though that that

00:16:04.408 --> 00:16:08.297
was not what the Humpback chub
necessarily needed because the Humpback

00:16:08.330 --> 00:16:12.956
chub is a spring spawner. So we were
not seeing warmer water in the spring

00:16:12.989 --> 00:16:17.177
, we were seeing warmer water in the
fall, but we were seeing warmer water

00:16:17.210 --> 00:16:20.297
nevertheless.

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So that was one thing that we didn't
fully understand and expect or

00:16:24.960 --> 00:16:28.907
appreciate when we started talking
about a temperature controlled device.

00:16:28.940 --> 00:16:35.366
Now, ironically, if you look at the
system in the Grand Canyon. Uh If you

00:16:35.399 --> 00:16:39.856
, if one were to consider the
continued trend or pattern of the lowering

00:16:39.889 --> 00:16:45.125
reservoir elevations and more warm
releases, one might even go as far as

00:16:45.158 --> 00:16:49.606
to say that maybe we do need a
temperature control device, but in fact, to

00:16:49.639 --> 00:16:53.145
cool it,

00:16:53.178 --> 00:16:58.326
um, can I ask you a question rich
about the, um Humpback chub spawning in

00:16:58.359 --> 00:17:03.976
the, uh LCR? Is that something that's
always occurred or is that uh

00:17:04.009 --> 00:17:09.024
something that developed after the,
after the dam was built as far as we

00:17:09.057 --> 00:17:14.966
know, it's, it's always occurred or at
least uh in recent history. The

00:17:14.999 --> 00:17:19.794
there were two brothers, the Cole
Brothers who are famous for their

00:17:19.827 --> 00:17:24.016
explorations in the Grand Canyon and
their photography in the Grand Canyon.

00:17:24.049 --> 00:17:28.456
And we have historic photographs of
the Cole Brothers going down to the

00:17:28.489 --> 00:17:31.986
little Colorado River at about the
time that the fish would be spawning

00:17:32.019 --> 00:17:36.436
and talking about that there were a
lot of fish in that system and they

00:17:36.469 --> 00:17:41.006
took their uh their, their fishing
poles and caught all they wanted for to

00:17:41.039 --> 00:17:47.217
eat. The earlier studies that were
done in about the 19 seventies also

00:17:47.250 --> 00:17:51.545
show that the fish were using that
system that way. So it's probably part

00:17:51.578 --> 00:17:56.617
of the historic use of the species
that is the little Colorado River. But

00:17:56.650 --> 00:18:00.976
we also suspect there was spawning
also occurring in the main stem of

00:18:01.009 --> 00:18:07.016
Colorado as well. That is prior to
closure of Glen Canyon Dam and in the

00:18:07.049 --> 00:18:12.867
sixties and then the releases of cold
water. So if anything did change, it

00:18:12.900 --> 00:18:16.936
was probably Humpback chub could no
longer spawn in the main stem, but

00:18:16.969 --> 00:18:20.825
they were still using the little
Colorado and that was providing the young

00:18:20.858 --> 00:18:27.367
to sustain the population. So the the
changes in the elevation of Lake

00:18:27.400 --> 00:18:33.706
Powell was one little bit of a
surprise for Mother Nature. The other which

00:18:33.739 --> 00:18:38.555
is somewhat related to that was also
declining reservoir elevation in Lake

00:18:38.588 --> 00:18:46.545
Mead which now increase the length of
the Colorado River into the Lake

00:18:46.578 --> 00:18:52.746
Mead Basin between about separation
rapid or separation rapid, which is

00:18:52.779 --> 00:18:57.785
where the uh the Powell historically
and the Howell Brothers historically

00:18:57.818 --> 00:19:05.818
left or abandoned the Powell
expedition between there for about uh some 65

00:19:06.318 --> 00:19:13.367
or so 70 miles all the way down to
Pearce ferry. And so now uh what was

00:19:13.400 --> 00:19:18.166
under uh Lake Powell and, and I
surveyed that area in the, in the nineties

00:19:18.199 --> 00:19:21.416
when it was in fact under Lake Powell
at the time. And there was a very,

00:19:21.449 --> 00:19:25.387
do you mean Lake Mead, I'm sorry, Lake
Mead, excuse me. Thank you. And

00:19:25.420 --> 00:19:29.607
there was a thick layer of sediment in
there that was the deposits of uh

00:19:29.640 --> 00:19:36.936
of, of Lake Mead. Now, uh with the
receding levels of Lake Mead, the

00:19:36.969 --> 00:19:42.486
Colorado River has carved out its
original channel and much of that

00:19:42.519 --> 00:19:50.226
historical habitat has been restored.
And in fact, the most um productive

00:19:50.259 --> 00:19:55.325
population that we have a Hump of
Humpback chub is probably in that what

00:19:55.358 --> 00:19:59.535
we referred to as the western Grand
Canyon, which is downstream of Diamond

00:19:59.568 --> 00:20:06.535
Creek and all the way down to about
Pierce ferry. So that area is, uh, if

00:20:06.568 --> 00:20:11.367
you go down to that area now and
sample some of the backwaters in that

00:20:11.400 --> 00:20:15.785
area, you, you'll catch primarily
native fish, not just Humpback chub, but

00:20:15.818 --> 00:20:18.776
flannel mouse suckers and blue head
suckers and speckled dace, The other

00:20:18.809 --> 00:20:23.506
species that are also there. And so
that has been another unexpected uh

00:20:23.539 --> 00:20:30.045
twist from mother nature, like I said,
uh where one can sit and plan all

00:20:30.078 --> 00:20:32.835
the things that you anticipate are
going to happen. But there's some

00:20:32.868 --> 00:20:38.526
things you just don't expect that that
will occur and take place.

00:20:38.559 --> 00:20:43.156
Um The other thing that you brought up
that I found fascinating is not

00:20:43.189 --> 00:20:50.647
only does nature surprise us, but um
when we make

00:20:50.680 --> 00:20:56.637
science is a practice of developing a
hypothesis, doing some research,

00:20:56.670 --> 00:21:02.236
developing a kind of a limited
knowledge base. And then in adaptive

00:21:02.269 --> 00:21:06.736
management, we go do a management
action, try to monitor it and find out

00:21:06.769 --> 00:21:11.217
if the response is what we expected.
So it's constant learning and what

00:21:11.250 --> 00:21:15.555
you with the, the stories that you
were telling us is about how fisheries

00:21:15.588 --> 00:21:21.035
biologists come up with a hypothesis
and then do some experiments and then

00:21:21.068 --> 00:21:25.736
learn that that's part of the story.
But it's more complicated and we're

00:21:25.769 --> 00:21:31.575
constantly developing a knowledge base
over time. That's, and, and it

00:21:31.608 --> 00:21:37.617
takes that opportunity to be able to
get involved at the, at the, at the

00:21:37.650 --> 00:21:44.045
beginning of planning something like
uh Glen Canyon Dam Eis and trying to

00:21:44.078 --> 00:21:48.936
structure those alternatives and doing
intense analysis of all the

00:21:48.969 --> 00:21:55.496
available data and testing of
hypotheses to try to anticipate or predict

00:21:55.529 --> 00:22:00.986
the response by resources, the
different management actions or scenarios.

00:22:01.019 --> 00:22:07.706
But it takes that opportunity and then
to go back years later and, and

00:22:07.739 --> 00:22:15.486
looking to see how right or wrong we
were. And, and it emphasizes that

00:22:15.519 --> 00:22:21.526
concept of Carl Walter's adaptive
management, whereby it's all a learning

00:22:21.559 --> 00:22:26.897
process. If one were to believe that
you could structure something in a

00:22:26.930 --> 00:22:31.446
way that's definitive with predictable
results and responses, that of

00:22:31.479 --> 00:22:37.217
course is not true at all. You learn
as you do, you learn as you go. And

00:22:37.250 --> 00:22:41.776
so that was that to me, that was the
biggest lesson from this, not only

00:22:41.809 --> 00:22:47.406
the way that resources responded to
the things that we predicted were

00:22:47.439 --> 00:22:52.377
going to happen, but also this, this
these tricks from Mother Nature also

00:22:52.410 --> 00:22:56.377
Mother Nature throwing little things
at us like climate change and

00:22:56.410 --> 00:23:00.847
lowering reservoir elevations or
different volumes of water coming down at

00:23:00.880 --> 00:23:06.315
different years or perhaps uh bigger
floods or smaller floods out of the

00:23:06.348 --> 00:23:10.147
Peria River or the little Colorado
River that delivered different amounts

00:23:10.180 --> 00:23:15.217
of sediment into the system. There was
always something going on that one

00:23:15.250 --> 00:23:19.906
somehow cannot always anticipate or or
make sure you cover as you're

00:23:19.939 --> 00:23:25.276
working on this. And so it really
does, especially as you get involved in

00:23:25.309 --> 00:23:29.347
a, as one gets involved in a project
from the beginning and you think

00:23:29.380 --> 00:23:33.016
you've really got this right? And then
you start looking at the responses

00:23:33.049 --> 00:23:36.887
down along the road a few years later
and then look back at it 20 or 30

00:23:36.920 --> 00:23:41.835
years later and you realize, wow, we
learned a lot, we got some things,

00:23:41.868 --> 00:23:45.795
right? We got some things not so
right. And there were some absolute

00:23:45.828 --> 00:23:49.127
surprises.

00:23:49.160 --> 00:23:55.347
So in addition to the surprises
related to the role of temperature, river

00:23:55.380 --> 00:24:02.176
, temperature on the viability and
health of the chubb uh population.

00:24:02.209 --> 00:24:08.226
There's also been some interesting
surprises in the role of predation.

00:24:08.259 --> 00:24:13.246
Some of our other interviewees talked
about how early hypotheses about

00:24:13.279 --> 00:24:18.026
predation evolved over time as we
learn more. Can you talk a little bit

00:24:18.059 --> 00:24:21.535
about that? Yeah,

00:24:21.568 --> 00:24:29.568
the the the Colorado river um is an
historic, an historical river in that

00:24:31.209 --> 00:24:37.226
it was it has been isolated from other
river, other surrounding or nearby

00:24:37.259 --> 00:24:43.906
river basins for probably the last uh
3 to 4 million years or more. The

00:24:43.939 --> 00:24:48.196
historical river in the upper basin is
very much like it has been for

00:24:48.229 --> 00:24:52.496
about that period of time through the
Grand through the Grand Canyon. Of

00:24:52.529 --> 00:24:57.976
course, we know that more recently as
the plateau rose and the river

00:24:58.009 --> 00:25:01.696
carved its way through the canyon and
captured some of the streams in the

00:25:01.729 --> 00:25:09.426
lower basin, we know that's AAA little
bit younger uh geologically.

00:25:09.459 --> 00:25:15.285
But because the Colorado River has
been isolated for so many years, the

00:25:15.318 --> 00:25:21.186
diversity of fish species in the
system has always remained quite low. And

00:25:21.219 --> 00:25:26.467
in fact, if you look at the main
Colorado river, not, not including the

00:25:26.500 --> 00:25:30.607
species that would be marine species
or that would use the estuary, not

00:25:30.640 --> 00:25:34.726
including those, there's only about 14
species that are native to the

00:25:34.759 --> 00:25:38.906
entire Colorado River basin. And if
you compare that to, for example, the

00:25:38.939 --> 00:25:43.676
Mississippi or the Missouri, where you
have hundreds of species, you can

00:25:43.709 --> 00:25:47.647
now begin to understand that you have
a very, very different, very unique

00:25:47.680 --> 00:25:54.065
evolutionary scheme that has taken
place in these systems, a situation

00:25:54.098 --> 00:25:59.785
where you have few predators and
therefore have few adaptive traits to be

00:25:59.818 --> 00:26:04.647
able to cope with predators. If they
get introduced into the system, alien

00:26:04.680 --> 00:26:10.496
predators from other systems, the the
species in the Colorado River are

00:26:10.529 --> 00:26:14.416
and, and all you have to do is look at
them and you can tell these are

00:26:14.449 --> 00:26:19.967
special, very, very special fish. They
are very uniquely adapted. You look

00:26:20.000 --> 00:26:24.887
at something like the Humpback chub.
It is a species that is very torpedo

00:26:24.920 --> 00:26:31.176
shaped to deal with high velocity
current. It is a species that has large

00:26:31.209 --> 00:26:37.956
falcate fins to be able to soar in
that current, not to necessarily swim

00:26:37.989 --> 00:26:41.637
into it at high velocity. In fact, the
Humpback chub is a very poor

00:26:41.670 --> 00:26:46.097
swimmer in laboratory experiments.
They're not even as good a swimmer as

00:26:46.130 --> 00:26:50.516
any salmon species or striped bass or
any river and species. But they're

00:26:50.549 --> 00:26:55.045
smart, they know how to deal with
these high currents by finding small

00:26:55.078 --> 00:27:00.906
eddies or small pockets of low
velocity. And, and III, I am fortunate

00:27:00.939 --> 00:27:05.916
enough to have been in the, I worked
with the species in the upper basin

00:27:05.949 --> 00:27:10.387
and to work with the species in the
lower basin in Grand Canyon where the

00:27:10.420 --> 00:27:16.877
water was clear and I could now see
the fish and it's fascinating to watch

00:27:16.910 --> 00:27:23.276
Humpback chub. Uh and how that fish is
able to maneuver through currents

00:27:23.309 --> 00:27:27.906
in the Grand Canyon. And I, and I'd
like to, to equate that somewhat to a

00:27:27.939 --> 00:27:35.416
raptor that is soaring on the edge of
a cliff or a rim and is using those

00:27:35.449 --> 00:27:40.035
thermals to maintain its position. And
all you see is it tweaks one wing a

00:27:40.068 --> 00:27:44.137
little bit or a feather and it's able
to stay there with relatively little

00:27:44.170 --> 00:27:48.736
energy expenditure. Well, Humpback
chub do the same thing except that

00:27:48.769 --> 00:27:53.976
they're in a water environment. And in
addition, the river also delivers

00:27:54.009 --> 00:27:59.285
food to them as they are sitting there
with little energy expenditure. So

00:27:59.318 --> 00:28:02.597
it's a fascinating species. They have
very uh they have deeply embedded

00:28:02.630 --> 00:28:09.967
scales. They have thick leathery skins
to resist the, the um the scouring

00:28:10.000 --> 00:28:18.000
of a sand laden system. They have a
flattened rostrum or, or the top of

00:28:18.529 --> 00:28:24.226
their head is flattened so that it
allows water to pass by. And also they

00:28:24.259 --> 00:28:28.575
have that hump, which is, which is the
origin of their name. What is the

00:28:28.608 --> 00:28:34.156
purpose of that? Hump? Robert Rush
Miller that who identified the fish or

00:28:34.189 --> 00:28:39.156
described the fish initially
taxonomical in 1946

00:28:39.189 --> 00:28:42.887
thought. And I, and I think there's a
lot to it that they, it's part of

00:28:42.920 --> 00:28:45.196
AAA hydrodynamic

00:28:45.229 --> 00:28:50.217
uh feature that enables or allows the
fish to maintain that position in

00:28:50.250 --> 00:28:54.387
the inner river current. There's no
bony structure in it at all. It's

00:28:54.420 --> 00:28:58.877
simply a fleshy structure. Unlike the
Razorback sucker. Razorback sucker

00:28:58.910 --> 00:29:03.805
has a in fact, it was also called the
Humpback sucker for many years. The

00:29:03.838 --> 00:29:08.377
razor back now it's called the
Razorback sucker. The Razorback sucker does

00:29:08.410 --> 00:29:13.906
in fact have a modified bony structure
that forms the razor or the hump,

00:29:13.939 --> 00:29:18.785
not so with Humpback chub, the
Humpback chub is a fleshy protrusion behind

00:29:18.818 --> 00:29:23.686
the head that takes place. So it helps
to stabilize. So if you look again

00:29:23.719 --> 00:29:28.676
at the different species, you can see
these adaptations, you see Razorback

00:29:28.709 --> 00:29:34.535
sucker with AAA hump on their back,
that if you look at it from the front

00:29:34.568 --> 00:29:41.256
appears to be this very nicely
designed hydrodynamic uh feature that would

00:29:41.289 --> 00:29:45.825
allow that fish to stabilize itself
and to maneuver around. It also has a

00:29:45.858 --> 00:29:51.627
very thick skin and also has fairly
large fins. And so these fish were

00:29:51.660 --> 00:29:56.656
very, very specifically and very
highly adapted to the environment. That

00:29:56.689 --> 00:30:04.689
is the Colorado River. Now along comes
uh well in the um

00:30:05.920 --> 00:30:08.736
in the 19

00:30:08.769 --> 00:30:13.246
starting in the 19 thirties, of
course, with Lake Mead and then through

00:30:13.279 --> 00:30:19.335
the Colorado river storage projects uh
with Glen Canyon Dam in 63 and then

00:30:19.368 --> 00:30:25.726
uh Flaming Gorge, 6263. And then
Navajo also, the states looked at at the

00:30:25.759 --> 00:30:29.785
formation of these reservoirs as a
great opportunity for recreational

00:30:29.818 --> 00:30:36.196
fisheries. And, and so with that, they
started introducing things like

00:30:36.229 --> 00:30:40.835
largemouth bass and Croppy and
bluegill and green sunfish and bullheads

00:30:40.868 --> 00:30:45.706
and fat minnows and red shiners, all
kinds of fish. And in fact,

00:30:45.739 --> 00:30:50.285
altogether, today, you've got 14 fish
that are native to the system and

00:30:50.318 --> 00:30:56.117
you've got upwards of about 30 to 35
that are alien or from other river

00:30:56.150 --> 00:31:01.627
basins and you have fish that are not,
are ill adapted. That is the

00:31:01.660 --> 00:31:06.847
Humpback Chub ill adapted to coping
with those with those alien predators

00:31:06.880 --> 00:31:11.815
or competitors. And there are also
vectors for disease and parasites as

00:31:11.848 --> 00:31:18.446
well. So, so now we go back to this
idea of a temperature control device

00:31:18.479 --> 00:31:23.496
and what protections the uh coal water
releases out of Glen Canyon Dam

00:31:23.529 --> 00:31:28.597
have provided to the Humpback chub.
Now we begin to better understand how

00:31:28.630 --> 00:31:34.295
that cold water has in fact been a
barrier or at least uh uh uh uh

00:31:34.328 --> 00:31:39.147
discouraged the invasion of many of
these alien fish that could have come

00:31:39.180 --> 00:31:43.276
up from Lake Mead or could have come
down from Lake Powell. Yes, they are

00:31:43.309 --> 00:31:48.545
in the system, but they are not
thriving as you might otherwise expect if

00:31:48.578 --> 00:31:55.107
it was a warm water system. So,
predation is a, is a key issue and it is

00:31:55.140 --> 00:32:00.065
in the Grand Canyon. Interestingly
enough, though, in the Grand Canyon

00:32:00.098 --> 00:32:06.996
predation is not necessarily from warm
water. Fish. Predation is

00:32:07.029 --> 00:32:12.377
principally from the cold water fish
that is rainbow trout and brown trout.

00:32:12.410 --> 00:32:17.887
And they were introduced for, uh,
fisheries based, uh, rec recreation,

00:32:17.920 --> 00:32:21.766
fisheries, recreation. Right? Yeah,
the, the, uh, those are not native to

00:32:21.799 --> 00:32:25.246
the rainbow trout.

00:32:25.279 --> 00:32:29.526
Both the rainbow trout and the brown
trout were introduced by the National

00:32:29.559 --> 00:32:36.436
Park Service in the 19 twenties into
initially into Bright Angel Creek.

00:32:36.469 --> 00:32:41.006
And of course, at that time,

00:32:41.039 --> 00:32:47.887
excuse me, the, the Colorado River was
a warm muddy Turbid River and yet

00:32:47.920 --> 00:32:52.815
there was Grand Canyon National Park
that had just been established. And

00:32:52.848 --> 00:32:56.535
so there was a need to have people
have some kind of recreational

00:32:56.568 --> 00:33:01.897
opportunity. You wouldn't imagine
fishing this dirty warm main stem

00:33:01.930 --> 00:33:06.156
Colorado River, but you would gain
enjoyment and in fact, the unique

00:33:06.189 --> 00:33:11.976
opportunity to fish for trout,
literally in the middle of the desert. And

00:33:12.009 --> 00:33:16.607
so the side streams in the side
streams exactly in places like Bright

00:33:16.640 --> 00:33:20.016
Angel Creek and Bright Angel Creek was
one of the places. In fact, it was

00:33:20.049 --> 00:33:25.357
the main place where trout were
brought in by the Park service. They

00:33:25.390 --> 00:33:30.916
brought them in and Clear Creek to
the, upstream from Bright they did,

00:33:30.949 --> 00:33:35.065
they did and in fact, did well, there
they did quite well. And in fact,

00:33:35.098 --> 00:33:39.565
there was a hatchery facility that was
set up at Bright Angel Creek to

00:33:39.598 --> 00:33:44.565
culture rainbow trout and brown trout.
And I'm curious, we have native

00:33:44.598 --> 00:33:49.766
trout in Arizona, like the Apache
trout. Um, I wonder, I, I've never heard

00:33:49.799 --> 00:33:54.335
anybody say that. Um, there were any
Apache trout native in these sides

00:33:54.368 --> 00:33:57.397
streams? Were there any trout in the
side streams or were they all

00:33:57.430 --> 00:34:05.430
imported the, um, the Apache trout and
the Gila trout are, are, um, are,

00:34:07.009 --> 00:34:11.845
were derived from a, uh,

00:34:11.878 --> 00:34:18.456
a fish that was more closely akin to
the salmon species as opposed to the

00:34:18.489 --> 00:34:25.666
mountain cutthroat trout. The patchy
trout and the Gila trout are not in

00:34:25.699 --> 00:34:30.276
tributaries of the Grand Canyon. They
are, they're native of the

00:34:30.309 --> 00:34:35.706
tributaries of the Gila river that
eventually does go into the Colorado

00:34:35.739 --> 00:34:41.945
river, but further downstream. And so,
uh, historically, and even today,

00:34:41.978 --> 00:34:46.845
we, we don't have Apache trout or Gila
trout in either headwaters of the

00:34:46.878 --> 00:34:52.345
Little Colorado River or in Havasu
Creek or any of the other, uh

00:34:52.378 --> 00:34:56.175
tributaries that come in on that site
or for that matter, on the other, on

00:34:56.208 --> 00:35:00.655
the north rim, either out of Bright
Angel or Shene or any of the other

00:35:00.688 --> 00:35:04.537
tributaries there as well. So, those
were outside of the system. So the

00:35:04.570 --> 00:35:11.175
fish that were introduced were, in
fact, uh, rainbow trout from, uh, from

00:35:11.208 --> 00:35:17.477
hat trees in California and then brown
trout from hatcheries in Michigan

00:35:17.510 --> 00:35:21.287
that eventually came from Europe
because the brown trout is a European

00:35:21.320 --> 00:35:24.756
species.

00:35:24.789 --> 00:35:29.986
And, um, you were talking about, um,
their role in, in predation on the

00:35:30.019 --> 00:35:36.967
humpback chub. Where does that come
in? Yeah. And so, um,

00:35:37.000 --> 00:35:41.856
the, uh, the, the rainbow trout of, of
course, has been concentrated

00:35:41.889 --> 00:35:46.827
principally in the tail water, uh, of,
of, of Glen Canyon Dam, The 15

00:35:46.860 --> 00:35:52.026
miles from the dam down to uh down to
Lee's ferry and that of course has

00:35:52.059 --> 00:35:57.706
become a world renowned blue ribbon
trout fishery. People come from all

00:35:57.739 --> 00:36:02.945
over the world to fish there. Uh There
have not been many brown trout in

00:36:02.978 --> 00:36:08.385
that system perhaps because the water
was too cold brown trout

00:36:08.418 --> 00:36:13.606
historically or that, that is after
the dam was completed in, in uh 1963

00:36:13.639 --> 00:36:18.345
brown trout were, were principally
concentrated around Bright Angel Creek.

00:36:18.378 --> 00:36:21.276
And that's of course where they were
introduced originally and there were

00:36:21.309 --> 00:36:25.327
some in the main stem as well. We
would catch brown trout at the mouth of

00:36:25.360 --> 00:36:30.787
the Little Colorado River which is
upstream of Bright Angel Creek and they

00:36:30.820 --> 00:36:34.796
were moving up there and then
evidently moving back and then spawning in

00:36:34.829 --> 00:36:40.537
Bright Angel Creek with the increasing
temperature

00:36:40.570 --> 00:36:45.566
as a result of lowered elevations in
Lake Powell and warmer water coming

00:36:45.599 --> 00:36:50.856
out of the dam, it has apparently
enabled or allowed brown trout to move

00:36:50.889 --> 00:36:57.006
around more in the main stem. So they
perhaps are not as closely tied to

00:36:57.039 --> 00:37:01.787
Bright Angel Creek. For example, as
they were historically, they can now

00:37:01.820 --> 00:37:06.577
start using the main stem more because
they're a warmer water fish species

00:37:06.610 --> 00:37:13.077
than say rainbow trout. Recently, we
have found brown trout up in Lee's

00:37:13.110 --> 00:37:19.247
ferry and in fact, in, in, in sizable
numbers and a concern is that brown

00:37:19.280 --> 00:37:24.217
trout may in fact be competitors and
predators for the rainbow trout at

00:37:24.250 --> 00:37:31.796
least very really. And then in 2017,

00:37:31.829 --> 00:37:37.787
the GC damp asked to convene a science
panel that was headed up by Mike

00:37:37.820 --> 00:37:43.885
Runge of the US, GS and Charles E
Kulick from GCMRC myself and other

00:37:43.918 --> 00:37:49.086
biologists in that program to look at
what alternatives might be available

00:37:49.119 --> 00:37:53.546
for controlling brown trout, removing
them and reducing that predation and

00:37:53.579 --> 00:37:58.186
competition threat, not just for
rainbow trout in the tail water, but the

00:37:58.219 --> 00:38:04.227
potential is that if brown trout were
to expand, then they could end up in

00:38:04.260 --> 00:38:10.046
prime Humpback chub habitat, which is,
uh, which is at the LCR river mile

00:38:10.079 --> 00:38:15.267
61. So about 75 miles or 76 miles
downstream from the dam. So that's a

00:38:15.300 --> 00:38:19.586
concern that we have now is the
potential for brown trout being a major

00:38:19.619 --> 00:38:23.307
predator in, in that system.

00:38:23.340 --> 00:38:29.146
I can remember, um, one of our
interviews, uh, somebody mentioned that, uh

00:38:29.179 --> 00:38:35.537
, early on the thinking was that both
species of trout were probably

00:38:35.570 --> 00:38:40.416
eating Humpback chub and depressing
the population. And after further

00:38:40.449 --> 00:38:45.017
research, it was determined that the
rainbow basically weren't and the

00:38:45.050 --> 00:38:49.376
brown trout were, is that correct in
your mind? There was, did we learn

00:38:49.409 --> 00:38:53.586
that? Yeah, there was, there was some
excellent work that was done by Mike

00:38:53.619 --> 00:39:00.017
Yard on looking at the effects of
predation by both species. And it

00:39:00.050 --> 00:39:02.936
followed up on some of the work that
we had done there earlier when we

00:39:02.969 --> 00:39:06.336
were doing the life history and
ecology studies on the Humpback chub. And

00:39:06.369 --> 00:39:12.626
what Mike found is that, uh, brown
trout, both species eat Humpback chub.

00:39:12.659 --> 00:39:17.026
They both will prey on them, but brown
trout eat them. As I recall,

00:39:17.059 --> 00:39:22.787
something like 3 to 4 times more,
they'll eat 3 to 4 times more. Humpback

00:39:22.820 --> 00:39:28.595
chub than rainbow trout dune. So the
pre so for one brown trout, you're

00:39:28.628 --> 00:39:32.037
gonna have a fish that would equal
maybe three or four rainbow trout in

00:39:32.070 --> 00:39:36.106
terms of the numbers of, of Humpback
chub that, that fish might eat. So

00:39:36.139 --> 00:39:40.905
predation was a, is a, is a real
problem, especially with brown trout. Um

00:39:40.938 --> 00:39:44.876
, the other species that we're seeing
in the system is, is the small mouth

00:39:44.909 --> 00:39:49.077
bass and we're especially concerned
about smallmouth bass because they in

00:39:49.110 --> 00:39:54.227
fact, are a cool water species. They
do tolerate cooler water than say

00:39:54.260 --> 00:39:59.717
large mouth bass or Cropper blue gills
or some of the warm water fish that

00:39:59.750 --> 00:40:05.296
fish has now recently gotten into the
Grand Canyon. To my knowledge, there

00:40:05.329 --> 00:40:08.106
is, there's no evidence of
reproduction in that system yet. But it's

00:40:08.139 --> 00:40:12.356
certainly a, a river that would be
suitable for reproduction by the by

00:40:12.389 --> 00:40:16.046
that species. So that's another one,
we're kind of keep an eye on our eye

00:40:16.079 --> 00:40:21.635
on and you expect them to be predators
on humpback. They are, they are

00:40:21.668 --> 00:40:27.296
intensive predators. In fact, um, the
upper Colorado river recovery

00:40:27.329 --> 00:40:33.037
program that manages these, these
endangered fish in the upper basin above

00:40:33.070 --> 00:40:38.736
Lake Powell currently spends about 40%
of its budget, controlling

00:40:38.769 --> 00:40:43.537
mechanically removing smallmouth bass
and northern pike in the upper

00:40:43.570 --> 00:40:50.256
Colorado river, specifically in the
northern pike in the Colorado river,

00:40:50.289 --> 00:40:55.396
they were introduced by the state of
Colorado into Elk Reservoir some

00:40:55.429 --> 00:40:59.796
years back and they escaped both
northern pike and Small Mount Bass. And

00:40:59.829 --> 00:41:05.626
in fact, today, there are guided tours
for fishing for northern pike and

00:41:05.659 --> 00:41:09.986
the Yampa River. You can hire a guide
out of Colorado to take you down the

00:41:10.019 --> 00:41:15.577
Yampa river and catch these £20
northern pike out of the Yampa river. Now

00:41:15.610 --> 00:41:21.287
, those fish are more aligned with
cold conditions, cold water conditions.

00:41:21.320 --> 00:41:24.006
You don't see them leaving the Yampa
much although we catch them in the

00:41:24.039 --> 00:41:29.126
Green River as well, but not as much.
But the, the the swam up bass is a

00:41:29.159 --> 00:41:33.486
much more uh plastic species in terms
of temperature. It can tolerate a

00:41:33.519 --> 00:41:38.686
big range of temperatures. And that's
one that I that I believe could be a

00:41:38.719 --> 00:41:43.135
real problem in the Grand Canyon in
years to come because it fills that

00:41:43.168 --> 00:41:47.046
intermediate niche between the cold
water species and the warm water

00:41:47.079 --> 00:41:53.079
species and could probably do quite
well in a place like the Grand Canyon.

00:41:53.728 --> 00:41:55.728
So, where are we at today? With the recovery of the Humpback chug? I heard

00:42:01.159 --> 00:42:06.816
recently that there was talk about
down listing it from endangered to

00:42:06.849 --> 00:42:11.456
threatened. Um, what's the status now?
And where do you think we're going

00:42:11.489 --> 00:42:15.956
in the near future? Yeah. The Humpback
chub is currently listed, of course

00:42:15.989 --> 00:42:20.606
as endangered. Um,

00:42:20.639 --> 00:42:26.405
it was brought into, it was
grandfathered into the endangered species Act

00:42:26.438 --> 00:42:31.836
in 1973. It was included in the
original list of endangered species in

00:42:31.869 --> 00:42:35.296
1966.

00:42:35.329 --> 00:42:41.776
Um And so it has been listed as
endangered for, you know, since

00:42:41.809 --> 00:42:48.267
fundamental. Yeah. Yeah, since that.
Yeah. Right. Half a century. Um

00:42:48.300 --> 00:42:52.717
because of the uh expanding numbers of
Humpback job that we see,

00:42:52.750 --> 00:42:57.856
especially in the Grand Canyon. The,
the increased abundance of Humpback

00:42:57.889 --> 00:43:02.106
chub in the Western Grand Canyon. And
how well the species is doing in the

00:43:02.139 --> 00:43:06.425
main ga in the main Grand Canyon. In
addition to the fish that are in the

00:43:06.458 --> 00:43:11.546
Little Colorado River, there are about
oh, about six or seven other, what

00:43:11.579 --> 00:43:15.307
we refer to as aggregations. They're
small groups of fish that are located

00:43:15.340 --> 00:43:19.997
usually in, in springs, warm water,
spring areas like fence vault at 30

00:43:20.030 --> 00:43:25.486
mile near Vys Paradise or around the
Little Colorado River, which is a

00:43:25.519 --> 00:43:33.206
seasonally warm system or around, uh,
perhaps, um, uh, Havasu Creek. I saw

00:43:33.239 --> 00:43:37.615
a bunch of Havasu creek mouth of
Havasu Creek and it was clear water. So I

00:43:37.648 --> 00:43:41.115
got to take pictures of them while I'm
standing kind of over them. And

00:43:41.148 --> 00:43:46.566
they're swimming around in that sandy
bottom. And in fact, many people who

00:43:46.599 --> 00:43:51.916
travel down the Grand Canyon now raft
down the Grand Canyon, uh, observe

00:43:51.949 --> 00:43:55.747
that one of the most common fish they
see is in fact, the Humpback chub,

00:43:55.780 --> 00:43:59.845
if there's scraps of food or whatever
fall in the river, they're the first

00:43:59.878 --> 00:44:03.986
ones there and they often almost are
begging like a bunch of little puppy

00:44:04.019 --> 00:44:10.066
dogs waiting to be fed. Uh They're
very social species, they usually uh

00:44:10.099 --> 00:44:15.195
move around in schools as groups of
individuals. And so, um that

00:44:15.228 --> 00:44:19.945
population of Humpback job is doing
quite well. In addition to that, there

00:44:19.978 --> 00:44:25.537
are also uh five other populations in
the upper Colorado River basin in

00:44:25.570 --> 00:44:29.807
Black Rocks, Westwater cataract
Canyon, desolation, Gray Canyon and Yampa

00:44:29.840 --> 00:44:35.166
Canyon. The Yampa Canyon population
has recently been declared as

00:44:35.199 --> 00:44:41.195
functionally extirpated. Uh We did a
species status assessment for the

00:44:41.228 --> 00:44:45.517
Humpback job about two years ago and
determined that the numbers of fish

00:44:45.550 --> 00:44:50.865
in that population were pretty much
gone. We recently convened a uh part

00:44:50.898 --> 00:44:54.916
of the Humpback Chub recovery team to
look at the prospect of trans

00:44:54.949 --> 00:44:58.896
locating Humpback chub back into the
Yampa River and establishing a

00:44:58.929 --> 00:45:03.615
population there, connected with Echo
Park and Whirlpool in the Green

00:45:03.648 --> 00:45:07.925
River which is below Flaming Gorge to
try to re-establish that population

00:45:07.958 --> 00:45:13.506
, the other populations are either
stable or perhaps in slight decline. So

00:45:13.539 --> 00:45:17.396
they're not doing quite as well,
perhaps as the Grand Canyon population,

00:45:17.429 --> 00:45:22.095
but they're, they're self sustained.
They produce young every year. Uh We

00:45:22.128 --> 00:45:27.106
see, you know, good numbers of them in
these populations. And so the

00:45:27.139 --> 00:45:32.706
service has decided that uh if we
examine the, the terms of the Endangered

00:45:32.739 --> 00:45:36.425
Species Act and what's defined as an
endangered species, one likely to go

00:45:36.458 --> 00:45:40.666
extinct within the foreseeable future,
that the impact job is, in fact,

00:45:40.699 --> 00:45:47.747
probably not that it is an AAA species
that faces threats. And so, uh

00:45:47.780 --> 00:45:53.626
perhaps the classification of
threatened is more appropriate. So the uh US

00:45:53.659 --> 00:45:58.365
fish and wildlife service here uh
about a month ago, which would be back

00:45:58.398 --> 00:46:06.398
in about February sometime 2020 2020.
Yeah, of this year, correct, uh

00:46:07.599 --> 00:46:15.599
initiated the process of a down list
proposal for the species. The

00:46:16.239 --> 00:46:20.967
proposal was published in the Federal
register about a, about a month ago

00:46:21.000 --> 00:46:26.956
, which would be about February 2020
and is open to comment, I think till

00:46:26.989 --> 00:46:34.217
the end of March 2020. If it is
determined that uh that it's appropriate

00:46:34.250 --> 00:46:39.526
to down list the species, the Humpback
chub could be down listed within,

00:46:39.559 --> 00:46:44.885
within the next year. Uh That would be
determined of course, as, as part

00:46:44.918 --> 00:46:49.595
of the ruling in the federal register.
So that, that's one that's one

00:46:49.628 --> 00:46:55.626
prospect. The likelihood I think of
that is pretty good. Um Given that the

00:46:55.659 --> 00:46:58.385
population is doing so well in the
Grand Canyon and given that the

00:46:58.418 --> 00:47:02.146
population in the upper basin are
holding their own, perhaps a little

00:47:02.179 --> 00:47:06.586
decline, perhaps in some years, they
go back up. And if we can get fish

00:47:06.619 --> 00:47:09.916
into the Yampa River, I think we'll be
in pretty good shape, but it

00:47:09.949 --> 00:47:14.615
certainly does not meet the definition
of endangered if you, if you look

00:47:14.648 --> 00:47:20.557
at it that way. Um There is, there is
another species that's also being

00:47:20.590 --> 00:47:24.807
considered now in the Grand Canyon.
And that's the Colorado pike minnow,

00:47:24.840 --> 00:47:30.586
Colorado pike. Minnow is also an
endangered species. And there is uh there

00:47:30.619 --> 00:47:37.376
is currently um an evaluation of, of
possibly reintroducing the Colorado

00:47:37.409 --> 00:47:42.236
pike metal into the Grand Canyon. It's
extirpated from the Grand Canyon

00:47:42.269 --> 00:47:47.345
right now. It has been extirpated from
the Grand Canyon since about 1975

00:47:47.378 --> 00:47:51.396
as a result of the changes in the
river due to the construction of Glen

00:47:51.429 --> 00:47:57.135
Canyon Dam or something else. Probably
all of the above where it was a

00:47:57.168 --> 00:48:01.135
highly, it it's a, it's what's known
as a PTA species. In other words,

00:48:01.168 --> 00:48:05.456
it's highly migratory within a given
river system. So we believe that that

00:48:05.489 --> 00:48:09.936
Colorado Pikemen at one time probably
migrated all the way from, say, Yuma

00:48:09.969 --> 00:48:13.916
Arizona, which is where it was warmer
and perhaps even went into the

00:48:13.949 --> 00:48:20.827
estuary to feed. And uh the evidence
is is strong that the fish got to

00:48:20.860 --> 00:48:25.497
about 6 ft or so in length and weighed
£100. Uh North America's largest

00:48:25.530 --> 00:48:29.416
minnow and we've got bone fragments
and remains that support that

00:48:29.449 --> 00:48:34.936
contention. Now, the biggest fish we
see are about 25 maybe £30. Uh So

00:48:34.969 --> 00:48:39.416
we're not quite seeing the, the large
fish now, perhaps because they're

00:48:39.449 --> 00:48:43.316
restricted to the upper basin and
perhaps because they don't have the full

00:48:43.349 --> 00:48:48.155
uh regime of temperature year round to
allow that growth. So we don't have

00:48:48.188 --> 00:48:55.135
any below lake uh uh Hoover Dam in
Lake. No, there are none below. Um

00:48:55.168 --> 00:49:00.945
There are none below Glen Canyon Dam.
Ok. At this time, everything is

00:49:00.978 --> 00:49:06.445
above Glen Canyon Dam except for the
small numbers that were introduced.

00:49:06.478 --> 00:49:09.666
They, they're not natural but they
were introduced into the Salt and

00:49:09.699 --> 00:49:14.307
Verde rivers, tributaries of the Gila
and those are known those are now

00:49:14.340 --> 00:49:19.586
currently called 10 J populations or
experimental non essential

00:49:19.619 --> 00:49:23.506
populations in others. They are there
just to have them there to maintain

00:49:23.539 --> 00:49:29.425
, but they're not part of recovery
targets at this time. So the idea is

00:49:29.458 --> 00:49:33.247
being entertained right now by A US
Fish and Wildlife Service and Arizona

00:49:33.280 --> 00:49:37.046
Game and Fish Department and the
National Park Service to perhaps look at

00:49:37.079 --> 00:49:43.146
the possibility of bringing Colorado
Pike Meadow into the Grand Canyon at

00:49:43.179 --> 00:49:49.037
least to have them there. The I I
think it's questionable whether all the

00:49:49.070 --> 00:49:52.977
life history requirements are there
for the species to be self sustained.

00:49:53.010 --> 00:50:00.077
I don't think so at this time, uh that
fish needs uh uh long rivers to

00:50:00.110 --> 00:50:06.307
migrate to spawn in clean headwater
areas, warm temperatures, the young

00:50:06.340 --> 00:50:13.467
drift, uh perhaps many miles up to
5060 miles or more into small sand

00:50:13.500 --> 00:50:17.526
backwaters where they can feed and
live for most of the, most of the rest

00:50:17.559 --> 00:50:21.706
of the year. It's a summertime spawner
they spawn in usually about late

00:50:21.739 --> 00:50:28.595
June, July. Sometime those, those key
life history elements are probably

00:50:28.628 --> 00:50:33.195
not present in the Grand Canyon, but I
think that that's still being

00:50:33.228 --> 00:50:37.175
looked at at least to have the species
there to say that they are

00:50:37.208 --> 00:50:42.155
someplace in the lower basin. Um

00:50:42.188 --> 00:50:49.405
So, so at this point in time, the um
again, the Humpback job is, is, is

00:50:49.438 --> 00:50:55.227
being proposed for down listing. I
think there's information that would

00:50:55.260 --> 00:50:58.945
warrant that at this time, we'll see
what the public decides and what

00:50:58.978 --> 00:51:06.095
others decide as well. If that, if
that down listing takes place, it

00:51:06.128 --> 00:51:13.287
really would not change much in terms
of how Glen Canyon Dam is operated.

00:51:13.320 --> 00:51:17.356
The difference between an endangered
species and a threatened species is

00:51:17.389 --> 00:51:20.066
,

00:51:20.099 --> 00:51:27.606
is small relative to section seven of
the, of the endangered Species Act.

00:51:27.639 --> 00:51:34.006
It can open some opportunities for
additional conservation measures. For

00:51:34.039 --> 00:51:38.057
example, there is a section in the
endangered Species Act called the four

00:51:38.090 --> 00:51:43.506
D rule. That is a provision that
allows the states now to become more

00:51:43.539 --> 00:51:47.986
active and more participant in part of
the conservation measures, it gives

00:51:48.019 --> 00:51:52.077
, for example, the states the
opportunity to define, take what is known as

00:51:52.110 --> 00:51:57.146
, take. In other words, how you can
take or kill or capture or maintain

00:51:57.179 --> 00:52:03.385
these individual individual fish. So
it might give some flexibility to

00:52:03.418 --> 00:52:10.037
management, which I think would be
good. Um Can can you say to what extent

00:52:10.070 --> 00:52:13.727
the improved

00:52:13.760 --> 00:52:20.695
health of the Humpback chub population
in the Grand Canyon is traceable to

00:52:20.728 --> 00:52:26.497
the Adaptive Management Program and
you know, changes in dam operations. I

00:52:26.530 --> 00:52:30.727
mean, how much of it is just
serendipity and how much of it is the results

00:52:30.760 --> 00:52:34.195
of our efforts to recover the species?

00:52:34.228 --> 00:52:40.077
That, that that is a thing of, of uh
scientist nightmare.

00:52:40.110 --> 00:52:47.595
Uh where one spends a lifetime trying
to be smart enough to come up with

00:52:47.628 --> 00:52:53.717
the right management actions and then
implements a program like Glen

00:52:53.750 --> 00:53:00.146
Canyon Dam Ltpis and then looks back
upon it 20 years later, whatever. And

00:53:00.179 --> 00:53:06.267
again, we're not that far away from it
yet, but we're going to be uh and

00:53:06.300 --> 00:53:10.365
you realize that many of the things
that you did either made a difference

00:53:10.398 --> 00:53:13.356
or didn't make a difference, most of
them perhaps didn't make much of a

00:53:13.389 --> 00:53:20.195
difference. And then the word
serendipity is perhaps the most the best

00:53:20.228 --> 00:53:26.006
word for that. How many things took
place naturally or normally part of

00:53:26.039 --> 00:53:32.796
the of the the expanded distribution
and abundance of the Humpback Chub is

00:53:32.829 --> 00:53:38.876
in fact, due to reoperation of Glen
Canyon Dam and the actions that were

00:53:38.909 --> 00:53:43.336
put in place by the federal Agencies
in Cooper operation with the States

00:53:43.369 --> 00:53:48.776
and other stakeholders. Part of that
recovery is directly attributed part

00:53:48.809 --> 00:53:53.967
of it. However, is in fact
serendipitous relative to the changing

00:53:54.000 --> 00:54:00.577
elevations of Lake Powell and Lake
Mead warmer releases from the dam and

00:54:00.610 --> 00:54:06.546
also re excavation of the historic
river channel downstream of Diamond

00:54:06.579 --> 00:54:11.956
Creek and all the way down to Pierce
ferry. Now, specifically, the things

00:54:11.989 --> 00:54:15.686
that were put in place that have
really helped. I think the Humpback chub

00:54:15.719 --> 00:54:20.506
is that um prior to 1995

00:54:20.539 --> 00:54:28.539
the Glen Canyon dam operation was um
was a

00:54:28.898 --> 00:54:35.606
a hydro power generation type facility
where hydropower is maximized by

00:54:35.639 --> 00:54:40.706
having flows as low as three or 5000
cubic feet per second in the middle

00:54:40.739 --> 00:54:45.327
of the night. And then at about four
o'clock in the morning, start ramping

00:54:45.360 --> 00:54:49.787
those releases up to say 30,000 cubic
feet per second, which is the

00:54:49.820 --> 00:54:55.756
capacity of the power plant. And you
would see then about a 20 ft increase

00:54:55.789 --> 00:55:00.276
in the elevation of the river right
there below the dam. And this of

00:55:00.309 --> 00:55:05.037
course would generate this uh
kinematic wave all the way downstream. And

00:55:05.070 --> 00:55:09.115
fundamentally, that was almost a daily
flushing of the Grand Canyon if you

00:55:09.148 --> 00:55:13.077
may, I mean to be a little extreme
perhaps, but that was kind of the

00:55:13.110 --> 00:55:17.086
effect. And so when I first got
involved, that was what was happening is

00:55:17.119 --> 00:55:21.296
we had these very, very high
fluctuations. And of course, people will tell

00:55:21.329 --> 00:55:25.077
stories about when you were down there
with the big rafts that you had to

00:55:25.110 --> 00:55:27.986
make sure you parked those boats in
such a place that you wouldn't be

00:55:28.019 --> 00:55:32.416
stranded on the beach for the next day
until those flows, you know, came

00:55:32.449 --> 00:55:40.449
back up. Um That operation of these
very, very large changes in flow and

00:55:42.369 --> 00:55:50.369
river elevation were probably um were
not beneficial to young Humpback job

00:55:50.619 --> 00:55:56.336
that used the shoreline for nursery
areas. The fish would come out of the

00:55:56.369 --> 00:56:01.506
little Colorado River as four or five
month old fish and then they would

00:56:01.539 --> 00:56:04.845
hang out along the shoreline, which
was the better place for them to

00:56:04.878 --> 00:56:11.227
escape predators and to find food with
flows going up and down. Even as

00:56:11.260 --> 00:56:16.997
far down as the LCR maybe as much as 4
5 6 ft or more, then you would have

00:56:17.030 --> 00:56:20.436
displacement of these fish and they
would either be displaced downstream

00:56:20.469 --> 00:56:25.227
or be displaced away from that cover
and be exposed to predation by, by

00:56:25.260 --> 00:56:30.017
another fish. So that was good that
the idea of what was known as the

00:56:30.050 --> 00:56:36.405
modified low fluctuating flow MLFF
that came about in, in uh in, in 1995

00:56:36.438 --> 00:56:41.526
basically as a result of those, those
studies that were done prior to that.

00:56:41.559 --> 00:56:47.336
Um That was good that and so that,
that made the, the habitat for the

00:56:47.369 --> 00:56:53.256
Humpback job a little bit more stable.
Now, admittedly, I was one of the

00:56:53.289 --> 00:56:57.095
biologists that were saying that was
saying at the time, in fact, you have

00:56:57.128 --> 00:57:01.727
to try to get those flows even more
stable because if you look at

00:57:01.760 --> 00:57:05.336
summertime in the Colorado River,
except for places where there's

00:57:05.369 --> 00:57:09.686
monsoonal storms that would be large
enough to increase flow by and large.

00:57:09.719 --> 00:57:12.546
The flow of the Colorado River during
the summertime was relatively

00:57:12.579 --> 00:57:16.885
stable. It didn't fluctuate and low,
correct low. And that's what brought

00:57:16.918 --> 00:57:22.006
about the low steady summer flow
concept, the flow that we had in 2000 to

00:57:22.039 --> 00:57:27.526
test that hypothesis. But what we
found out and thanks to some of the work

00:57:27.559 --> 00:57:32.776
done by Bill Pine and and others is
that in fact, the Humpback job was

00:57:32.809 --> 00:57:38.586
quite plastic in terms of its ability
to be able to move with those flows

00:57:38.619 --> 00:57:43.425
and use those tailless slopes. If you
look at the at the slopes in Grand

00:57:43.458 --> 00:57:46.767
Canyon, for example, downstream of the
little Colorado River where you

00:57:46.800 --> 00:57:51.807
have young Humpback chub, they are, in
fact, slopes of Talus that are

00:57:51.840 --> 00:57:56.807
continuous rock and boulder mixture
all the way up the slope. So all the

00:57:56.840 --> 00:58:00.486
humpback job has to do is just move
with the water and it's at a new

00:58:00.519 --> 00:58:05.736
interface that is still that boulder
tailless habitat where you can still

00:58:05.769 --> 00:58:09.615
use those areas for different kind in
the back water. You get behind in

00:58:09.648 --> 00:58:14.425
the little little eddies and
backwaters and little cubby holes in and

00:58:14.458 --> 00:58:21.776
between these boulders. So the large
fluctuations that we saw prior to

00:58:21.809 --> 00:58:26.936
MLFF were probably not good for the
humpback job. The more modified

00:58:26.969 --> 00:58:31.026
fluctuations have probably helped to
benefit the species and in fact

00:58:31.059 --> 00:58:34.967
probably do help even stimulate maybe
some production along those

00:58:35.000 --> 00:58:39.327
shorelines when you have water moving
around the way it does. So that,

00:58:39.360 --> 00:58:43.566
that, that did help out. The other
thing where we think there was quite a

00:58:43.599 --> 00:58:48.486
bit of benefit is, is there was, in
fact, mechanical predation, mechanical

00:58:48.519 --> 00:58:56.519
predator removal in the Grand Canyon.
Um, even before the Ltpis, where we

00:58:57.639 --> 00:59:01.385
were removing brown trout and rainbow
trout from the system, as well as

00:59:01.418 --> 00:59:06.546
other species removing channel catfish
or carp from the little Colorado

00:59:06.579 --> 00:59:11.615
River as well. Are catfish also
predators on Humpback? Absolutely. Very

00:59:11.648 --> 00:59:17.977
much so that not Carp because, well,
carp we know are, are voracious

00:59:18.010 --> 00:59:24.896
predators of fish eggs. Oh, ok. And
I've watched, uh, uh, red shiners

00:59:24.929 --> 00:59:29.287
spawning in Spencer Creek, which is
the lower end of Grand Canyon. And

00:59:29.320 --> 00:59:33.425
then as the red shiners were spawning
early one morning, it wasn't but

00:59:33.458 --> 00:59:40.146
five minutes. And here comes a, an
entire herd of Humpback, excuse me, of

00:59:40.179 --> 00:59:44.977
carp, common carp that came up and
just vacuum that entire area for eggs.

00:59:45.010 --> 00:59:48.706
So they, they're not native either.
That's correct. Yeah. And that's

00:59:48.739 --> 00:59:52.787
another species that we may
underestimate in terms of their effect to

00:59:52.820 --> 00:59:56.267
these native fish is how, how much
effect they may have on eggs and on

00:59:56.300 --> 01:00:02.526
larvae and, and their predation there
as well. So, um so that, so that was

01:00:02.559 --> 01:00:08.405
another thing is, is modifying those
fluctuating flows, doing some

01:00:08.438 --> 01:00:13.006
predator control to reduce the, the
the predation on those fish. The other

01:00:13.039 --> 01:00:18.626
, the other thing that probably did
help Humpback chub was um

01:00:18.659 --> 01:00:26.659
was these high flow experiments that
provided uh large sandy beaches and

01:00:27.059 --> 01:00:33.936
deposits in the large recirculating
eddy complexes of the Grand Canyon.

01:00:33.969 --> 01:00:40.126
And as part of that recirculating
complex, of course, what happens is that

01:00:40.159 --> 01:00:44.736
the water is laden with sediment
because it, it is a higher volume, higher

01:00:44.769 --> 01:00:52.769
velocity. Uh The the the base flows
may be at uh 1512, 1510, 15, 12,000

01:00:53.628 --> 01:00:56.945
cubic feet per second. With a high
flow experiment, you're going up to

01:00:56.978 --> 01:01:01.977
45,000, which is the, the 30,000 out
of the power plant and then the

01:01:02.010 --> 01:01:07.695
15,000 out of the bypass valves. So
when you've got 45,000 CFS going down

01:01:07.728 --> 01:01:14.376
the system, you are lifting,
activating, energizing the sediment in the

01:01:14.409 --> 01:01:19.115
system suspending it. And then when it
gets to these large recirculating

01:01:19.148 --> 01:01:25.416
eddies, it slows down and drops out in
the eddy was part of that large

01:01:25.449 --> 01:01:30.115
sandy beach. There is the recurrent
channel which is that little stream of

01:01:30.148 --> 01:01:33.845
high velocity water that goes right
against the bank. And behind that

01:01:33.878 --> 01:01:39.236
sandbar, that recurrent channel forms
a backwater, which is very nice

01:01:39.269 --> 01:01:44.345
habitat for fish. And while Humpback
chub don't necessarily use those that

01:01:44.378 --> 01:01:49.537
often. They are there. Nevertheless.
And the high flow experiments do help

01:01:49.570 --> 01:01:53.967
to provide that environment for the
fish. But also other native species

01:01:54.000 --> 01:01:57.327
like flannel mouse suckers and blue
head suckers and speckled dace do use

01:01:57.360 --> 01:02:01.477
those habitats. So it has helped. So
those are some of the things that the

01:02:01.510 --> 01:02:04.967
reoperation has done to benefit the
fish. But like I said, many of the

01:02:05.000 --> 01:02:09.066
others are like you said,
serendipitous because they are tied to mother

01:02:09.099 --> 01:02:14.115
nature and climate change and
availability of water in different years.

01:02:14.148 --> 01:02:20.925
That that's great explanation. Thank
you. Um You did some studies of the

01:02:20.958 --> 01:02:27.066
early high flow experiments to
determine whether they were being effective

01:02:27.099 --> 01:02:32.026
or not. Can you talk about how the
science and our understanding of the

01:02:32.059 --> 01:02:36.526
impacts of those high flow experiments
has evolved from the, the first one

01:02:36.559 --> 01:02:40.856
was sometime in the 19 nineties,
right? And that's when you were looking

01:02:40.889 --> 01:02:45.925
at that. And you have a couple of
publications from 1999 and 2001 on that.

01:02:45.958 --> 01:02:50.686
Yes. So how did our understanding of
those high flow experiments evolve

01:02:50.719 --> 01:02:56.436
over time? Well, the, the first
experiment of course was the 1996 control

01:02:56.469 --> 01:03:00.416
Flood. We called it The Control Flood
through Grand Canyon. And of course

01:03:00.449 --> 01:03:07.776
, uh I was fortunate enough to edit a
book with uh Bob Webb Jack Schmidt

01:03:07.809 --> 01:03:15.066
and Dick Marzo called the 1996 Control
Flood in the Grand Canyon. And it's

01:03:15.099 --> 01:03:19.595
available through the Geophysical
Union. It's available on the internet.

01:03:19.628 --> 01:03:23.747
And that archived many of the studies
that were done at that time and what

01:03:23.780 --> 01:03:28.747
we found out about a high flow
experiment. Now, prior to that, it was, it

01:03:28.780 --> 01:03:35.017
was called the uh beach habitat
building flow BHBF. That was a terminology

01:03:35.050 --> 01:03:37.836
that was supposed to be descriptive of
what it was supposed to do. And

01:03:37.869 --> 01:03:42.336
that was to beach, to build habitat,
to build beaches, beach habitat,

01:03:42.369 --> 01:03:47.986
building flow. But the history of that
is, is, is I think even more

01:03:48.019 --> 01:03:54.856
interesting. The na when, when Dave
Wagner was uh head of the Glen Kenyon

01:03:54.889 --> 01:04:00.146
environmental studies, G ce s, this is
all the way back into the um the

01:04:00.179 --> 01:04:08.179
mid eighties. He asked the National
Academy of Sciences to do a review of

01:04:09.099 --> 01:04:14.577
studies and the program G CS in the
Grand Canyon. And of course, that was

01:04:14.610 --> 01:04:22.610
just after the high flow of 1983 and
84 where the capacity of lake Paul

01:04:23.309 --> 01:04:27.526
was practically exceeded. And there
were these emergency releases. You,

01:04:27.559 --> 01:04:35.006
you can read about it in uh the book
by Kevin Fedarko the Emerald Mild,

01:04:35.039 --> 01:04:38.977
correct, did an excellent job of
documenting what was happening at that

01:04:39.010 --> 01:04:45.546
time. But um what the National Academy
of Sciences concluded after that,

01:04:45.579 --> 01:04:50.787
after that experience with those high
flows was that in fact, high flows

01:04:50.820 --> 01:04:55.945
are bad for the Grand Canyon because
in fact, they transport large amounts

01:04:55.978 --> 01:05:02.827
of sediment out, out of the system,
correct? And so the initial thought

01:05:02.860 --> 01:05:06.175
was oh my goodness, we can't allow
these high flows to take place in the

01:05:06.208 --> 01:05:11.796
Grand Canyon. A second review by the
National Academy of Sciences. A few

01:05:11.829 --> 01:05:16.467
years later said, no, there's perhaps
more to it than that. Perhaps we can

01:05:16.500 --> 01:05:22.626
use certain releases from Glen Canyon
Dam to in fact, suspend that

01:05:22.659 --> 01:05:27.896
sediment and not transport all of it
out of the system. But in fact, and

01:05:27.929 --> 01:05:31.497
train some of it in these large
recirculating eddies. And it was people

01:05:31.530 --> 01:05:37.506
like Jack Schmidt and other scientists
that said this is a way perhaps to

01:05:37.539 --> 01:05:42.787
preserve sediment, sand in the Grand
Canyon as beaches for river runners,

01:05:42.820 --> 01:05:48.436
for camping and a substrate for
riparian habitat for all the way from

01:05:48.469 --> 01:05:54.436
Southwest Willow flycatchers to
reptiles and lizards and all kinds of

01:05:54.469 --> 01:06:02.469
animals that rely on those riparian
areas. And so in the um leading up to

01:06:02.750 --> 01:06:09.767
the 1995 EIS, the concept was, was
developed uh of beach habitat building

01:06:09.800 --> 01:06:15.606
flows bhbfs. And as a result of that,
uh the Secretary of Interior

01:06:15.639 --> 01:06:21.456
approved a high flow release, which
was, which was really significant

01:06:21.489 --> 01:06:28.477
because it in fact um was a release
that not only involved the full power

01:06:28.510 --> 01:06:33.115
plant capacity of 30,000 cubic feet
per second but also involved the

01:06:33.148 --> 01:06:37.856
bypass valves. Now, the bypass valves
are what are known as the jet tubes

01:06:37.889 --> 01:06:44.066
do not have hydropower generating
facilities. And so there was in fact,

01:06:44.099 --> 01:06:48.247
the cost associated with that and the
lost hyder power revenue cost do you

01:06:48.280 --> 01:06:56.280
mean? Exactly. And so the first uh
nine, the 1996 experiment went for, uh

01:06:58.070 --> 01:07:01.606
gosh, almost almost two weeks. As I
recall, it went for a long period of

01:07:01.639 --> 01:07:05.445
time. But again, we learned a lot from
it because what we learned is, is

01:07:05.478 --> 01:07:08.537
in fact the majority of that sediment
was moved in about the first two or

01:07:08.570 --> 01:07:12.477
three days. So we learned that you
don't need to have these for a very

01:07:12.510 --> 01:07:16.497
long period of time. You can only, you
can have them for just 48 to say 96

01:07:16.530 --> 01:07:19.916
hours, something like that. And that's
more than enough to, to move that

01:07:19.949 --> 01:07:23.517
sediment. Um

01:07:23.550 --> 01:07:31.550
So, so the uh so what happened is that
um as that understanding was

01:07:32.478 --> 01:07:40.155
becoming better known than there was
eventually a protocol developed for

01:07:40.188 --> 01:07:47.517
releasing water from Glen Canyon Dam.
That was both a fall HFV and a

01:07:47.550 --> 01:07:53.747
spring HFV for the possibility of
releasing water depending on when

01:07:53.780 --> 01:07:59.967
sediment was available. Now, it just
so happens that the major sources of

01:08:00.000 --> 01:08:03.776
sediment to Grand Canyon now, because
all the sediment from the upper

01:08:03.809 --> 01:08:07.807
basin is trapped in Lake Powell. The
major sources of sediment are of

01:08:07.840 --> 01:08:13.885
course the Perla River which is 15
miles downstream from the dam and the

01:08:13.918 --> 01:08:18.607
little Colorado River which is about
76 miles downstream from the dam. The

01:08:18.640 --> 01:08:24.527
Perla River is principally a fall
monsoonal storm driven system. So that,

01:08:24.560 --> 01:08:29.567
that sediment is usually driven in the
late uh is usually transported in

01:08:29.600 --> 01:08:34.616
the late summer time in about July
August. During the monsoonal storms,

01:08:34.649 --> 01:08:39.476
the LCR, the little Colorado River
further downstream is a spring flood

01:08:39.509 --> 01:08:44.844
system so that sediment is available
at a different time of year.

01:08:44.877 --> 01:08:50.424
Initially, the high flow experiments
were being done in the springtime

01:08:50.457 --> 01:08:54.924
with the idea that it was more
simulating the natural hydra that you know

01:08:54.957 --> 01:09:00.715
, those were spring floods.
Eventually, it became better understood that

01:09:00.748 --> 01:09:04.054
the majority of sediment in fact would
be available from the PA because it

01:09:04.087 --> 01:09:07.856
was right there just downstream from
the dam and you could release it in a

01:09:07.889 --> 01:09:12.316
timely way that you could take
advantage of that large amount of sediment.

01:09:12.349 --> 01:09:17.965
Besides the majority, many of those
large recirculating complexes that

01:09:17.998 --> 01:09:22.825
entrained that sediment are located
upstream of the Little Colorado River.

01:09:22.858 --> 01:09:29.455
So it's that area around from Vys
Paradise on down all the way down

01:09:29.488 --> 01:09:32.776
pretty much to the LCR. That's, that's
where a lot of the benefit would

01:09:32.809 --> 01:09:40.809
come. Although there are other areas
downstream as well now. Um So HFES

01:09:41.489 --> 01:09:47.135
then high flow experiments became
initially were spring high flow

01:09:47.168 --> 01:09:55.168
experiments and then became fall high
flow experiments. Now, most recently

01:09:55.259 --> 01:09:59.006
and, and here's, here's adaptive
management coming into play, right? Where

01:09:59.039 --> 01:10:04.416
most recently the people that are
looking at uh production of insects in

01:10:04.449 --> 01:10:09.326
the Grand Canyon and production of
algae and everything else are saying,

01:10:09.359 --> 01:10:13.857
we're seeing a real decline in our
food base in the Grand Canyon and we

01:10:13.890 --> 01:10:19.916
think part of the reason is it's tied
to these fall high flow experiments

01:10:19.949 --> 01:10:23.737
where uh where in the fall when you
have a high flow experiment, you have

01:10:23.770 --> 01:10:27.996
got 40,000 or so cubic feet per second
coming out of the dam, you've got a

01:10:28.029 --> 01:10:33.027
real scouring effect, especially on
that uh where most of that primary

01:10:33.060 --> 01:10:37.706
production takes place. And that's in
that 15 mile reach of Lee's ferry.

01:10:37.739 --> 01:10:43.286
So if you scour that production at
that time of year, you are now at the

01:10:43.319 --> 01:10:48.666
point in the, in the year to where
you've got a low sun angle and you

01:10:48.699 --> 01:10:52.726
don't have as much potential
photosynthetic production taking place as you

01:10:52.759 --> 01:10:57.595
might otherwise. And then you've got
the entire winter period where that

01:10:57.628 --> 01:11:02.476
community does not have a chance to
recover and have, you know, and be

01:11:02.509 --> 01:11:06.626
back and productive again as you might
otherwise think. So that's one of

01:11:06.659 --> 01:11:10.717
the things we're learning the fall
hfes may be beneficial for storage of

01:11:10.750 --> 01:11:14.866
sediment because it maximizes that
sediment availability. But it also

01:11:14.899 --> 01:11:19.796
might be ne negative or detrimental
to, to production in the system which

01:11:19.829 --> 01:11:24.006
drives the whole the whole food basin
system. We've been hearing about low

01:11:24.039 --> 01:11:30.826
bug flows lately. Can you explain
that? Yeah. Um

01:11:30.859 --> 01:11:37.796
The combination of cold water releases
through the Grand Canyon

01:11:37.829 --> 01:11:43.956
in a uniform manner without seasonal
warming because the water is always

01:11:43.989 --> 01:11:50.527
coming out or, you know, at one about
one temperature before, before Lake

01:11:50.560 --> 01:11:56.765
Paul went down, it was always at about
8 to 10 °C. Now it's between 1012,

01:11:56.798 --> 01:12:01.467
maybe 13, but it's not warming up to
say what the river used to be

01:12:01.500 --> 01:12:09.425
historically, which was 25 °C. So you
don't see that seasonal warming that

01:12:09.458 --> 01:12:17.458
combined with the fluctuating flows
that we see has precluded

01:12:18.399 --> 01:12:23.576
the establishment of certain species
of invertebrates, especially may

01:12:23.609 --> 01:12:29.595
flies, stone flies, catus flies,
species that fish food, exactly, fish

01:12:29.628 --> 01:12:34.976
food, the the basis of production in
the system. Um,

01:12:35.009 --> 01:12:40.336
species of insects that are what we
refer to as multi volte species or

01:12:40.369 --> 01:12:46.027
species that require both a warm
period and a very cold period to complete

01:12:46.060 --> 01:12:50.226
their life cycle. So those species are
not in the system. They are Univ

01:12:50.259 --> 01:12:56.226
species which can, which can survive
and exist in places like we have in

01:12:56.259 --> 01:13:02.866
the Grand Canyon now. And so the idea
came up, uh, gentleman named Ted

01:13:02.899 --> 01:13:06.647
Kennedy, who's with GCMRC, came up
with the idea of what are known as the

01:13:06.680 --> 01:13:11.345
bug flows. So that on weekends,
especially when there's not that much

01:13:11.378 --> 01:13:15.996
power demand and we have more
flexibility in, in dam operations, then then

01:13:16.029 --> 01:13:20.277
perhaps instead of fluctuating, then
you run the flow at a certain level

01:13:20.310 --> 01:13:24.937
and then you allow these bugs to crawl
up on the rocks and deposit their

01:13:24.970 --> 01:13:29.765
eggs and keep the eggs wet, so they
don't dry out and die. And then you

01:13:29.798 --> 01:13:34.406
have hatching of those and you've got
at least some reinstatement of some

01:13:34.439 --> 01:13:39.116
of that historical bug community so to
speak is that working it, it

01:13:39.149 --> 01:13:42.687
appears to be working. The experiments
are limited, of course, at this

01:13:42.720 --> 01:13:46.916
time because they're being done on a
limited time basis. But they do

01:13:46.949 --> 01:13:52.666
appear to be working, they do appear
to be, there are more of certain

01:13:52.699 --> 01:13:57.706
species of insects in the system that
are potentially food for the fish.

01:13:57.739 --> 01:14:03.055
And so that in and of itself is
working. However, the issue of Fall hfes

01:14:03.088 --> 01:14:07.496
and their scouring effect on
production is still one that's being

01:14:07.529 --> 01:14:13.675
considered and talked about. And in
fact, there is consideration of now

01:14:13.708 --> 01:14:18.366
switching perhaps back to spring HBs
or switching back and forth perhaps

01:14:18.399 --> 01:14:24.317
and not having these continuously
during the fall. So, um as I understand

01:14:24.350 --> 01:14:28.326
it, they won't even do an HFE if they
haven't determined that a certain

01:14:28.359 --> 01:14:32.336
amount of sediment has come down one
of those two tributaries and is

01:14:32.369 --> 01:14:37.416
available to push down the Colorado.
So some years they won't do, they do

01:14:37.449 --> 01:14:41.506
one every fall or do some falls. They
don't do an HFE at all if there

01:14:41.539 --> 01:14:44.796
isn't enough sediment. Yeah. There,
there's two factors that determine the

01:14:44.829 --> 01:14:50.416
, the um uh an HFE taking place. One
of course is the availability of

01:14:50.449 --> 01:14:56.076
water availability of enough volume to
be able to release that volume that

01:14:56.109 --> 01:15:00.296
may not otherwise be part of normal
operations. And then the second is the

01:15:00.329 --> 01:15:04.166
availability of the sediment, the
amount of sediment in the system. And of

01:15:04.199 --> 01:15:07.916
course, that's monitored on an ongoing
basis to make sure that there's

01:15:07.949 --> 01:15:11.595
enough sediment there that if you do
an HFV, you're going to have some

01:15:11.628 --> 01:15:17.055
benefit from it. So, yes, there are
some times when an HFE is not

01:15:17.088 --> 01:15:23.107
authorized, authorized or suitable
because of the lack of sediment.

01:15:23.140 --> 01:15:27.546
How about if we take a short break now
and then come back in about five

01:15:27.579 --> 01:15:32.446
minutes? Ok. Pausing, recording,

01:15:32.479 --> 01:15:35.836
resuming, recording.

01:15:35.869 --> 01:15:40.737
Um One of the topics we touched on in
the first half of the interview was

01:15:40.770 --> 01:15:46.826
the topic of mechanical removal of
predatory fish that, uh, impact the

01:15:46.859 --> 01:15:51.906
chubb population, brown trout in
particular, but also rainbow. Um, can you

01:15:51.939 --> 01:15:56.647
talk a little bit about how mechanical
remo, what role mechanical removal

01:15:56.680 --> 01:16:02.217
has played in fish management and what
happened when it was adopted for

01:16:02.250 --> 01:16:09.527
the Glen Canyon, um Adaptive
Management program? Yeah. Uh, the, the, the

01:16:09.560 --> 01:16:14.206
threat of predation especially and to
a certain degree competition on

01:16:14.239 --> 01:16:19.046
especially the Humpback chub was a
common theme across the Colorado River

01:16:19.079 --> 01:16:26.265
basin in all populations. One of the
biggest concerns was the numbers of

01:16:26.298 --> 01:16:31.437
young fish, especially that would be
lost to, uh, things like smallmouth

01:16:31.470 --> 01:16:36.675
bass or largemouth bass or channel
catfish or other species, literally

01:16:36.708 --> 01:16:43.206
eating those young, removing them from
the population. So, um, the idea,

01:16:43.239 --> 01:16:46.987
there were, there were many ideas that
were, that were discussed in terms

01:16:47.020 --> 01:16:52.876
of how to manage these non native
species and one of the, of course most

01:16:52.909 --> 01:16:56.656
outstanding and most direct was the
concept of mechanical removal. That is

01:16:56.689 --> 01:17:01.397
you simply just put people out there
in electro fishing boats or nets or

01:17:01.430 --> 01:17:05.425
whatever gears you can use and catch
as many of those non native fish as

01:17:05.458 --> 01:17:10.956
you can and remove them from the
system with presumably the desired

01:17:10.989 --> 01:17:14.015
outcome that you would have fewer of
them. And therefore you would have

01:17:14.048 --> 01:17:18.336
less predation and fewer of the native
fish, more than more of the native

01:17:18.369 --> 01:17:25.885
fish surviving and, and helping to
sustain the population. So, um, in the

01:17:25.918 --> 01:17:28.326
Grand Canyon,

01:17:28.359 --> 01:17:34.496
going back to pretty much pretty much
after the 90 1995 biological opinion

01:17:34.529 --> 01:17:39.107
and the 1996 record of decision on the
final environmental impact

01:17:39.140 --> 01:17:43.836
statement. A a at that time, one of
the biggest threats to the Humpback

01:17:43.869 --> 01:17:51.305
job was seen as, uh, as predation and
because we recognized it was a cold

01:17:51.338 --> 01:17:58.786
water system, we acknowledge the
possibility of, of competition and

01:17:58.819 --> 01:18:04.765
predation from warm water fish. Um,
but we, we knew that there weren't

01:18:04.798 --> 01:18:08.286
that many. We knew that the cold water
was pretty much limiting the

01:18:08.319 --> 01:18:13.126
populations in the Grand Canyon, but
we began to recognize that, uh,

01:18:13.159 --> 01:18:17.607
perhaps the biggest threat was
predation and competition, especially

01:18:17.640 --> 01:18:21.656
predation from rainbow trout and brown
trout. And like I mentioned earlier

01:18:21.689 --> 01:18:26.737
, uh, Mike Yard did I think a very
good, uh, piece of work there when he

01:18:26.770 --> 01:18:30.607
looked at those proportions of fish
that were being taken by the two

01:18:30.640 --> 01:18:35.135
species and found out that the big
predator was, was brown trout. However

01:18:35.168 --> 01:18:42.086
, um, rainbow trout were still far,
far more abundant than brown trout in

01:18:42.119 --> 01:18:44.647
the Grand Canyon

01:18:44.680 --> 01:18:48.885
Carl Walters brought up the idea that
if you look genetically and

01:18:48.918 --> 01:18:54.876
historically, at the rainbow trout, it
really is the, uh, progeny of an

01:18:54.909 --> 01:18:59.175
anatomist species, right? A species
that moves or migrates. So we should

01:18:59.208 --> 01:19:03.317
not discount the possibility that
fish. And at that time, the rainbow

01:19:03.350 --> 01:19:08.595
trout were in fact being actively
introduced every year by Arizona Game

01:19:08.628 --> 01:19:12.015
and Fish department to sustain the
fishery because the water was literally

01:19:12.048 --> 01:19:16.836
too cold for rainbow trout to
reproduce in the Grand Canyon. And the

01:19:16.869 --> 01:19:22.717
fluctuations were so great that it
stranded and isolated their eggs. So

01:19:22.750 --> 01:19:27.217
the population of trout in the Grand
Canyon was not self sustainable until

01:19:27.250 --> 01:19:31.296
we went to modified low fluctuating
flows. Those high fluctuating flows

01:19:31.329 --> 01:19:36.046
were simply not allowing trout to
sustain themselves in the Grand Canyon.

01:19:36.079 --> 01:19:40.836
So once, once that population became
more self sustainable in the Lee

01:19:40.869 --> 01:19:46.286
ferry reach, then we started to see
some of those younger trough moving

01:19:46.319 --> 01:19:51.717
downstream. And we were concerned that
that movement downstream. All they

01:19:51.750 --> 01:19:58.607
have to do is go from the, from Lee's
ferry down to the LCR is 61 miles.

01:19:58.640 --> 01:20:03.397
So they don't have to go very far to
be in Humpback chub heaven, let's say

01:20:03.430 --> 01:20:11.430
Humpback chub territory. Um And so we,
uh, came up with the idea that one

01:20:12.319 --> 01:20:19.006
of the things we could do was set up a
uh uh lease ferry to, to Badger the

01:20:19.039 --> 01:20:26.027
Badger Creek removal as, as being
intensive removal in that area. At key

01:20:26.060 --> 01:20:29.946
times of the year, when we thought
that those rainbow trout would be

01:20:29.979 --> 01:20:35.156
moving downstream to so to speak, to
intercept them before they would

01:20:35.189 --> 01:20:40.086
reach the little Colorado River. So it
actually was, it was called the

01:20:40.119 --> 01:20:45.527
Pera the Badger uh proposal per he had
a badger mechanical removal

01:20:45.560 --> 01:20:49.317
proposal. And there were some
experiments that were done. There was some

01:20:49.350 --> 01:20:53.885
removal. There was a, a complete uh in
fact, there was a high uh an E A an

01:20:53.918 --> 01:20:58.616
environmental assessment done on that
coordinate by Mike Runge to look at

01:20:58.649 --> 01:21:05.217
that prospect of doing that and then
linking that to the 1995 EIS

01:21:05.250 --> 01:21:13.027
as a way to authorize that removal.
Now, research on that and the proposal

01:21:13.060 --> 01:21:18.226
for that was before the 1995 I was
being developed at the time, it was

01:21:18.259 --> 01:21:23.357
being developed and immediately after
and it was after correct. Right. And

01:21:23.390 --> 01:21:31.095
then starting in the early two
thousands, then the idea was floated that

01:21:31.128 --> 01:21:35.925
it could also be just targeting and
removing fish trout that is from

01:21:35.958 --> 01:21:40.277
around the little Colorado river
because the trying to intercept them in

01:21:40.310 --> 01:21:46.326
that pie. A badger reach was perhaps
more chance than something more

01:21:46.359 --> 01:21:49.876
certain. And and instead go to the
source itself, go to the end point and

01:21:49.909 --> 01:21:54.687
remove them there. So that became uh a
program that was designed as a

01:21:54.720 --> 01:21:59.567
multiyear experiment to where there
were, there were multiple trips. I

01:21:59.600 --> 01:22:03.607
think there was something like six or
eight removal trips through that

01:22:03.640 --> 01:22:08.836
area uh, of the little Colorado River,
both upstream and below. Uh the

01:22:08.869 --> 01:22:14.265
little Colorado River where electro
fishing boats were removing trout in

01:22:14.298 --> 01:22:18.956
mass and just taking them from the
system.

01:22:18.989 --> 01:22:24.135
Now, that became complicated to a
certain degree because you had two

01:22:24.168 --> 01:22:27.326
issues. One is what do you do with
them? Once you pull them from the

01:22:27.359 --> 01:22:32.777
system, you have a mass of, uh, you
know, several, yeah, several £100 of

01:22:32.810 --> 01:22:36.206
fish protein. What do you do with it?
The park service would not let us

01:22:36.239 --> 01:22:41.067
grind them up and put them back into
the system. We thought of burying

01:22:41.100 --> 01:22:45.166
them in some riverside pits or
something. But that didn't go over very

01:22:45.199 --> 01:22:49.166
well either. So someone came up with
the idea of something called the

01:22:49.199 --> 01:22:53.095
Basam Attic, which was basically a
huge grinder and you just put them

01:22:53.128 --> 01:22:58.885
through a grinder and then put all
that, pour all that soup into. Um, I

01:22:58.918 --> 01:23:04.265
think there were like 30 gallon
barrels that were put on boats and then

01:23:04.298 --> 01:23:08.277
floated out all the way to Diamond
Creek and then taken out and made

01:23:08.310 --> 01:23:13.476
available for fertilizer and they were
used by the Wallabies. And I think

01:23:13.509 --> 01:23:19.226
others too as fertilizer. Eventually
it became, we had a, we eventually

01:23:19.259 --> 01:23:24.506
had a surplus of fish soup that no one
had any further use for those. So

01:23:24.539 --> 01:23:29.055
we didn't quite know what to what to
do. Meantime, the Native American

01:23:29.088 --> 01:23:35.116
tribes and, and rightfully so um had
concerns about taking life in the

01:23:35.149 --> 01:23:39.717
Grand Canyon, what was referred to the
sanctity of life which we of course

01:23:39.750 --> 01:23:45.196
wanted to make sure was respected. So,
um so those removal that those

01:23:45.229 --> 01:23:49.937
removal experiments went on for, I
think about three years and the

01:23:49.970 --> 01:23:54.317
information was written up and what we
found is that they were effective

01:23:54.350 --> 01:24:00.226
as long as that removal was ongoing.
But as soon as it was relieved for

01:24:00.259 --> 01:24:06.487
about a year or so, you started to see
the influx of additional fish to

01:24:06.520 --> 01:24:12.607
repopulate that area. And I'm talking
specifically rainbow trout. And so

01:24:12.640 --> 01:24:16.777
it became questionable whether that
was in fact a sustainable management

01:24:16.810 --> 01:24:20.576
action, whether you could keep doing
that or whether, you know, maybe

01:24:20.609 --> 01:24:25.256
something else would be better or
maybe so. So then we started thinking,

01:24:25.289 --> 01:24:31.576
ok, so what would the Humpback chub
population need to reach? How many,

01:24:31.609 --> 01:24:38.515
how many adults, 5000, 10,000, 15,000
or more in order to be able to

01:24:38.548 --> 01:24:44.217
sustain a certain amount of predation
by rainbow trout? And so that became

01:24:44.250 --> 01:24:50.366
, then we developed triggers around
that. We said, ok, we won't implement

01:24:50.399 --> 01:24:55.376
non native fish removal until it's
necessary to do so. And the trigger

01:24:55.409 --> 01:25:00.467
will be not just the abundance of
rainbow trout in that area, not how many

01:25:00.500 --> 01:25:06.116
fish are there, but also how low that
Humpback chub population is and how

01:25:06.149 --> 01:25:10.476
much, how susceptible it might be to
effective predation. So those two

01:25:10.509 --> 01:25:14.796
factors came into effect and that was
all, eventually, that was all part

01:25:14.829 --> 01:25:21.777
of the consideration of the, of the
2016 LT MP. But by the time we got

01:25:21.810 --> 01:25:27.467
there, people like Mike Yard had done
these studies on the relative effect

01:25:27.500 --> 01:25:31.397
of predation by brown trout versus,
versus rainbow trout. And it was

01:25:31.430 --> 01:25:34.976
determined that in fact, probably
brown trout were perhaps a bigger threat

01:25:35.009 --> 01:25:42.515
than rainbow trout. So instead of
implementing the pet a badger strategy

01:25:42.548 --> 01:25:48.265
or removal around the LCR, it was
decided instead to go to Bright Angel

01:25:48.298 --> 01:25:53.175
Creek and try to go to the source of
brown trout that were primarily

01:25:53.208 --> 01:25:59.036
spawning, uh, in Bright Angel Creek.
And you see these £10 brown trout and

01:25:59.069 --> 01:26:02.166
we've caught them off the mouth of
Bright Angel Creek that go into Bright

01:26:02.199 --> 01:26:06.515
Angel Creek to spawn. So they're using
the, the main river a lot like

01:26:06.548 --> 01:26:11.036
humpback job. They're living and being
sustained in the main Colorado

01:26:11.069 --> 01:26:16.726
river. And every year in the fall,
they fall spawners, they migrate and go

01:26:16.759 --> 01:26:20.226
into Bright Angel Creek to spawn. And
then that's where their younger hats

01:26:20.259 --> 01:26:24.456
and that's where they come out and
that's where you intercept them. And so

01:26:24.489 --> 01:26:31.967
in about 2000 and I probably have the
year wrong here, but about 2000 and

01:26:32.000 --> 01:26:38.175
12 or so, uh, there was a, the park
service together with, uh, other

01:26:38.208 --> 01:26:46.208
biologists put a, um, of a fish wear
at the mouth of Bright Angel Creek

01:26:46.239 --> 01:26:51.217
that was literally catching all of
the, all the fish going into Bright

01:26:51.250 --> 01:26:57.666
Angel Creek and they removed, uh,
excuse me, large numbers of rainbow

01:26:57.699 --> 01:27:02.456
trout and brown trout at that. We so
rainbow trout we're spotting also in

01:27:02.489 --> 01:27:06.805
bright rainbow trout. We're also using
that and going into it. And then

01:27:06.838 --> 01:27:12.397
most recently in about the last now
five years, the park service has

01:27:12.430 --> 01:27:16.046
implemented a program to where they go
into Bright Angel Creek and

01:27:16.079 --> 01:27:21.717
literally just remove the trout
directly from Bright Angel Creek, both

01:27:21.750 --> 01:27:26.916
both brown trout and rainbow trout. I
just reviewed a manuscript submitted

01:27:26.949 --> 01:27:31.416
to one of the Canadian journals that
reports that the effect of that or

01:27:31.449 --> 01:27:37.277
result of that and the no, the, the
non native fish have declined by like

01:27:37.310 --> 01:27:43.595
75 or 80%. I mean, it's, it's really
had an effect.

01:27:43.628 --> 01:27:51.628
Excuse me. Mhm. Maybe, let's pause,

01:27:53.579 --> 01:28:01.579
recording resumes. So the, um, the
decision was made then to, uh, move the

01:28:03.088 --> 01:28:08.476
mechanical removal to Bright Angel
Creek and the park service, uh, was the

01:28:08.509 --> 01:28:14.996
lead in this, in this effort. Um,
there was a, uh, a fish weir that was

01:28:15.029 --> 01:28:21.967
set up in about 2010, 2012 that was
intercepting these large spawning

01:28:22.000 --> 01:28:25.647
adults that were coming out in from
the main stem, both rainbow trout and

01:28:25.680 --> 01:28:31.147
, and, and uh, brown trout. I remember
we were handling £10 brown trout in

01:28:31.180 --> 01:28:34.706
the main channel just off of Bright
Angel Creek. So these fish were coming

01:28:34.739 --> 01:28:40.586
into Bright Angel Creek and spawning
there. Um That was not without

01:28:40.619 --> 01:28:44.406
controversy either because there were
fishermen, a select group of

01:28:44.439 --> 01:28:51.476
fishermen that had recognized this for
some years and would make annual

01:28:51.509 --> 01:28:58.067
annual treks to hiking down the trail
to Phantom Ranch to fish. Those big

01:28:58.100 --> 01:29:01.866
rainbow, those big brown trout,
especially in the fall. The weather was

01:29:01.899 --> 01:29:06.345
nice, it was cool, it wasn't so hot,
hiking up and down that trail. And so

01:29:06.378 --> 01:29:11.305
the B A trail and so that became a bit
of a controversy that those fish

01:29:11.338 --> 01:29:16.296
were being removed from that system. I
recently received the manuscript uh

01:29:16.329 --> 01:29:22.765
from one of the Canadian uh journals,
uh where uh Brian Healy from the

01:29:22.798 --> 01:29:27.027
National Park Service and Charles Yule
from GCMRC have put together a

01:29:27.060 --> 01:29:31.366
paper evaluating the results of those,
those removals in there. And it,

01:29:31.399 --> 01:29:37.095
and it was, it's absolutely amazing
how well that has worked. Um They've

01:29:37.128 --> 01:29:42.607
removed something about 75 to 80% of
the, of the trout in that system,

01:29:42.640 --> 01:29:47.956
mostly rainbow trout, but browns as
well. And the, the native fish

01:29:47.989 --> 01:29:51.345
population, the flannel mouse sucker,
flannel mouse suckers, blue head

01:29:51.378 --> 01:29:56.135
suckers. There are no humpback chub in
Bright Angel, but those other

01:29:56.168 --> 01:30:01.976
native species have just increased,
something like 400% of their, of their

01:30:02.009 --> 01:30:08.067
former abundance. So, so it has worked
pretty well, but once again, once

01:30:08.100 --> 01:30:12.217
you remove that effort, the question
becomes, how long will it be before

01:30:12.250 --> 01:30:17.817
that system becomes re invaded? So,
again, there are costs associated with

01:30:17.850 --> 01:30:22.385
management actions that have to be
considered whenever one implements

01:30:22.418 --> 01:30:26.897
those actions and looks at the
prospect of having to do that, you know,

01:30:26.930 --> 01:30:32.616
for whatever long it takes or perhaps
to do them periodically to just

01:30:32.649 --> 01:30:37.796
maintain some balance of what's going
on. So, so the the issue of non

01:30:37.829 --> 01:30:42.086
native fish and especially mechanical
removal has been a major issue in

01:30:42.119 --> 01:30:47.126
the Grand Canyon and it has been at
the center of uh of some of the

01:30:47.159 --> 01:30:52.576
proposed management policies, but also
it, it has been controversial um in

01:30:52.609 --> 01:30:57.996
a number of different areas where
that's going to go. Now, um I think

01:30:58.029 --> 01:31:02.246
there are some different prospects or
possibilities of what may happen

01:31:02.279 --> 01:31:08.496
next. The system because of the way
that GCMRC and the Arizona Game and

01:31:08.529 --> 01:31:12.467
Fish Department are currently sampling
through the Grand Canyon, the

01:31:12.500 --> 01:31:19.206
system is currently essentially being
monitored so that any uh sudden

01:31:19.239 --> 01:31:23.246
explosion, you might say, or expansion
of a given species, whether it's

01:31:23.279 --> 01:31:30.107
small mouth bass or something else
should be detectable before perhaps it

01:31:30.140 --> 01:31:35.265
gets, it gets too far. And, and I
think the strategy now is to try to get

01:31:35.298 --> 01:31:40.055
at something like that if it were to
happen to try to get into those areas

01:31:40.088 --> 01:31:45.046
and mechanically remove before that
expansion takes place. So I, I think

01:31:45.079 --> 01:31:48.746
that that system is being monitored
right now. But I would suspect small

01:31:48.779 --> 01:31:54.595
mouth bass may be the next problematic
species in the Grand Canyon. So, as

01:31:54.628 --> 01:32:00.515
far as you know, right now, 2019 2020
there isn't an active mechanical

01:32:00.548 --> 01:32:07.826
removal program, but it's still a
possibility and may become necessary for

01:32:07.859 --> 01:32:12.196
smallmouth bass in the future. The the
mechanical removal program in

01:32:12.229 --> 01:32:17.336
Bright Angel Creek is is ongoing, it
is ongoing. So that's still going on.

01:32:17.369 --> 01:32:25.277
There's also some removal uh in Havasu
Creek, which is one of the places

01:32:25.310 --> 01:32:29.116
that Humpback chub have been
translocated to hump back job were

01:32:29.149 --> 01:32:35.086
translocated into uh Shino Creek and
then Havasu Creek to try to establish

01:32:35.119 --> 01:32:39.626
additional populations. But as far as
I know at this point in time, those

01:32:39.659 --> 01:32:43.576
are the only two places where there is
mechanical removal. And, and I

01:32:43.609 --> 01:32:46.916
think the approach is, you know, given
the native American concerns, the

01:32:46.949 --> 01:32:51.515
approach is to try to improve the
Humpback chub population sufficiently so

01:32:51.548 --> 01:32:57.425
that it is able to sustain a certain
level of predation and, and you don't

01:32:57.458 --> 01:33:01.857
have to go in and mechanically remove.
But so, so now what's going on in

01:33:01.890 --> 01:33:07.006
the Grand Canyon as a result of this
uh Brown trop management team that we

01:33:07.039 --> 01:33:13.555
convene in 4017,

01:33:13.588 --> 01:33:20.925
there are just being put in place uh
incentivized removal programs at

01:33:20.958 --> 01:33:28.958
least ferry. So, for example, the, um
the program will pay uh eee

01:33:29.500 --> 01:33:34.626
essentially a bounty on Brown trout
that, that are brought in by, by

01:33:34.659 --> 01:33:39.555
fishermen, by anglers. So that if you
bring in x number of brown trout,

01:33:39.588 --> 01:33:43.527
you, you, you can make some money
fishing basically, if you're, if you're

01:33:43.560 --> 01:33:48.256
good at it and can catch those fish
and have fresh fish for dinner and

01:33:48.289 --> 01:33:51.897
have fresh fish for dinner. Exactly.
You, you basically just take them to

01:33:51.930 --> 01:33:55.737
a person who's, who's, uh, examining
those fish and verifies that, that's

01:33:55.770 --> 01:33:59.607
what they are. And you, yeah, you keep
them and take them home. Now,

01:33:59.640 --> 01:34:03.446
that's just being implemented right
now. The, the interesting thing about

01:34:03.479 --> 01:34:07.015
it is that you can actually, and this
is part of what the Brown Trout

01:34:07.048 --> 01:34:12.656
Management team did is from an
economic perspective, you can actually look

01:34:12.689 --> 01:34:16.937
at the cost of mechanical removal that
is putting crews out there with

01:34:16.970 --> 01:34:22.546
electro fishing boats repeatedly
removing these fish from the system and

01:34:22.579 --> 01:34:27.746
compare that to the cost of an, an
incentivized program. And it's actually

01:34:27.779 --> 01:34:32.187
potentially cheaper to implement an
incentivized program. Even though you

01:34:32.220 --> 01:34:37.595
may be paying people, you may pay
them, uh, you know, 5 $10 a fish,

01:34:37.628 --> 01:34:42.015
whatever it might be. And then
periodically you might offer, uh, for AAA

01:34:42.048 --> 01:34:48.015
tagged fish. Let's say that that
that's $100 fish or maybe even $1000 fish.

01:34:48.048 --> 01:34:51.366
So, you incentivize people to continue
to try to remove those fish, to

01:34:51.399 --> 01:34:55.317
try to catch them. So those are some,
you know, new ideas that we're

01:34:55.350 --> 01:34:59.446
coming up with as a way to deal with
this mechanical removal or this non

01:34:59.479 --> 01:35:03.876
native fish issue? Are you aware of
any objections by the Havasupai tribe

01:35:03.909 --> 01:35:09.675
of mechanical removal of trout in
Havasu Creek? That, that is a sensitive

01:35:09.708 --> 01:35:14.006
issue at this time, I haven't been
directly involved with that program. I

01:35:14.039 --> 01:35:18.536
know that there are some concerns
about that. I really couldn't answer

01:35:18.569 --> 01:35:24.626
that at this time. I haven't had
recent involvement with that.

01:35:24.659 --> 01:35:30.746
Well, thank you for going back over
that topic with us again. Um Can you

01:35:30.779 --> 01:35:38.425
uh tell us who you think the most
important researchers and the most

01:35:38.458 --> 01:35:43.277
important participants in the adaptive
management program have been over

01:35:43.310 --> 01:35:49.277
time should be called out for their
long term high quality work. Well,

01:35:49.310 --> 01:35:54.515
from my perspective, of course, I, I
look more at the scientists in the

01:35:54.548 --> 01:35:58.345
program, perhaps more so than the
managers or administrators, not that

01:35:58.378 --> 01:36:02.546
they not that there aren't people
there that have done excellent work in

01:36:02.579 --> 01:36:06.015
terms of facilitating the science and
some of the research that's been

01:36:06.048 --> 01:36:11.546
taking place. But, but II, I think
that um certainly when I first got

01:36:11.579 --> 01:36:17.336
involved in the program in 1989 Dave
Wagner was a an instrumental person

01:36:17.369 --> 01:36:23.425
in terms of being able to bring
together scientists under the Glen Canyon

01:36:23.458 --> 01:36:30.406
environmental studies, the G CE S at
that time. Um After that, uh the

01:36:30.439 --> 01:36:35.826
program transitioned as a result of
the um of the Grand Canyon uh

01:36:35.859 --> 01:36:40.595
Protection Protection Act. Thank you.
Uh transitioned into the GCMRC, the

01:36:40.628 --> 01:36:46.777
, the uh Grand Canyon Monitoring and
Research Center. Um

01:36:46.810 --> 01:36:53.555
That program then was what Facilli
facilitated people like Carl Walters to

01:36:53.588 --> 01:36:59.635
come into the program. And Carl Carl
really, I think shook up the

01:36:59.668 --> 01:37:03.687
scientific community in Grand Canyon
because we thought we were pretty

01:37:03.720 --> 01:37:10.305
darn good at what we were doing. Carl
made us realize that we could do

01:37:10.338 --> 01:37:14.345
more, much more, especially
introducing this concept of adaptive

01:37:14.378 --> 01:37:19.036
management and how that really works
into uh being able to work in the

01:37:19.069 --> 01:37:23.277
system. So, so Carl fundamentally came
in and said, OK, what are your

01:37:23.310 --> 01:37:27.135
hypothesis about how you think the
system works? You think it's

01:37:27.168 --> 01:37:32.086
temperature that affects Humpback
chub? All right, then, then look at it,

01:37:32.119 --> 01:37:36.756
investigate it, look at different
options, look at opportunistic uh

01:37:36.789 --> 01:37:42.626
warming periods. We had 2005, for
example, that uh where the, where the

01:37:42.659 --> 01:37:49.666
release of the dam in 2005 was very
similar to a two unit T CD. So we had

01:37:49.699 --> 01:37:53.027
in some ways natural experiments that
were taking place right in front of

01:37:53.060 --> 01:37:56.857
our eyes, but we weren't seeing it
that way. So he made us better

01:37:56.890 --> 01:38:01.756
understand the opportunities that were
available in the system at the time

01:38:01.789 --> 01:38:05.976
and, and, and how to implement those
experiments and then how to evaluate

01:38:06.009 --> 01:38:12.246
them over time under the concept of
condition dependency. So that if, if

01:38:12.279 --> 01:38:17.376
we wanted to, to implement an an
experiment, we had to realize that the

01:38:17.409 --> 01:38:21.116
condition in the Grand Canyon, whether
it's water availability or

01:38:21.149 --> 01:38:25.897
temperature or whatever else, climate
change was not going to be the same

01:38:25.930 --> 01:38:32.586
every year. So, so it was basically
conducting a huge outdoor experiment

01:38:32.619 --> 01:38:38.515
over which you have little control
over environmental variables. And so in

01:38:38.548 --> 01:38:44.196
order to deal with that, he, you know,
proffered the idea of of condition

01:38:44.229 --> 01:38:49.175
dependent experiments whereby you, you
conduct experiments when the

01:38:49.208 --> 01:38:52.845
conditions are suitable for doing
that. And in years when you can't do

01:38:52.878 --> 01:38:57.607
that, you don't. So your condition,
your your sampling design may be a

01:38:57.640 --> 01:39:02.746
rather expanded matrix that has
probability of occurrence associated with

01:39:02.779 --> 01:39:06.467
a certain volume of water or a certain
temperature that you may be trying

01:39:06.500 --> 01:39:10.857
to test, but you're not going to be
able to do it every year. So Carl was

01:39:10.890 --> 01:39:15.717
significant in terms of introducing
some very novel, very, very, I think,

01:39:15.750 --> 01:39:20.666
very good ideas in terms of
understanding the science. Better. Carl also

01:39:20.699 --> 01:39:25.586
uh brought with him and enabled us to
also have access to people like Bill

01:39:25.619 --> 01:39:30.226
Pine. Uh Carl of course, with was
with, with the University of British

01:39:30.259 --> 01:39:34.156
Columbia in Vancouver. Bill Pine was
with the University of Florida at

01:39:34.189 --> 01:39:40.586
Gainesville. So Bill brought forward
concepts that we of how we better

01:39:40.619 --> 01:39:45.717
understand young Humpback chub
survival. He initiated some what are known

01:39:45.750 --> 01:39:49.737
as the near shore ecology studies in
the Grand Canyon. They were looking

01:39:49.770 --> 01:39:54.527
at the Humpback chub coming out of the
little Colorado River and what they

01:39:54.560 --> 01:39:57.987
were doing to survive in the main
stem, how they were using those tailless

01:39:58.020 --> 01:40:03.857
slopes for protection for food
availability and so on. And so Bill was

01:40:03.890 --> 01:40:08.546
instrumental in that as well as other
things. He, he introduced technology

01:40:08.579 --> 01:40:15.385
like uh like laser ablation technology
that is taking a uh an otolith, the

01:40:15.418 --> 01:40:20.496
inner ear bone of a fish of a humpback
chub, the inner ear, of course, is

01:40:20.529 --> 01:40:25.116
one of the first calcified parts of a
fish when they're born, they have

01:40:25.149 --> 01:40:28.256
inner ears, they have odorless when
they're born. So it's a complete

01:40:28.289 --> 01:40:36.289
record of the uh of the life of the
fish. And those Odalis establish um

01:40:36.338 --> 01:40:40.576
daily growth rings that you can track
and you can look at like the growth

01:40:40.609 --> 01:40:46.036
rings on a tree and they also have
broader, wider annual growth rings. And

01:40:46.069 --> 01:40:50.147
so you have a, a record that you can
go back and look at. Now if you take

01:40:50.180 --> 01:40:56.086
a laser and take uh samples of the
different parts in the life of that

01:40:56.119 --> 01:40:59.857
ring where you know how old the fish
is when it experienced certain things

01:40:59.890 --> 01:41:07.166
, you can then trace back what um what
environments it occupied by looking

01:41:07.199 --> 01:41:12.217
at isotope ratios, for example. So you
can tell when the fish left the

01:41:12.250 --> 01:41:16.437
little Colorado River, you can tell
what habitats they were using in the

01:41:16.470 --> 01:41:21.397
main stem, whether they were using
warm near shore habitats backwaters or

01:41:21.430 --> 01:41:26.357
the main channel or other experiences
or whether they were going into the

01:41:26.390 --> 01:41:30.586
main stem turning around and going
back up into the little Colorado River

01:41:30.619 --> 01:41:35.305
as part of a, a uh an archive of the
life history of the species in the

01:41:35.338 --> 01:41:41.506
system. So it was, it was these things
that we had not thought of before

01:41:41.539 --> 01:41:46.095
and that you need external scientists
like this to, to introduce these

01:41:46.128 --> 01:41:53.726
ideas and these concepts. Um One of
Carl Walters, uh A and Bill Pine's

01:41:53.759 --> 01:41:58.937
students was a, was a man named Lou
Coggins who got his phd under Bill

01:41:58.970 --> 01:42:05.687
Pine and, and Carl and Lou now
introduced new analytical techniques for us.

01:42:05.720 --> 01:42:11.175
Now, you had two fundamentally, two
scientists, Carl Walters and Bill

01:42:11.208 --> 01:42:18.496
Pine with very strong uh marine fish
backgrounds

01:42:18.529 --> 01:42:22.946
and marine fisheries is so much
further ahead in terms of analytical

01:42:22.979 --> 01:42:27.126
techniques than freshwater fisheries
because they deal with large fish

01:42:27.159 --> 01:42:30.406
populations, they deal with unknowns,
they deal with uncertainties, they

01:42:30.439 --> 01:42:36.536
deal with fish that are being reported
from large fishing boats, not with

01:42:36.569 --> 01:42:40.046
a lot of Mark recapture opportunities.
They're not dealing with small

01:42:40.079 --> 01:42:42.826
streams and lakes, they're dealing
with something the size of the Pacific

01:42:42.859 --> 01:42:49.616
Ocean. So they have to have much
better developed uh analytical skills.

01:42:49.649 --> 01:42:55.217
And so with their help, we had Lou
Coggins come in and redo our Mark

01:42:55.250 --> 01:42:59.286
recapture program of how we were
estimating the numbers of Humpback chub

01:42:59.319 --> 01:43:03.476
that were in the Grand Canyon. And he
developed a wonderful Mark recapture

01:43:03.509 --> 01:43:06.906
model with the help of both, you know,
especially Carl Walters but Bill

01:43:06.939 --> 01:43:14.939
Pine as well. Um, another student of,
uh, of Carl's was, um, was, um, uh,

01:43:17.289 --> 01:43:22.946
in addition to Lou Coggins was, uh,
uh, I, I'll have to think of his name

01:43:22.979 --> 01:43:28.656
here in a little bit, but he also
brought in, um, a, a wealth of knowledge

01:43:28.689 --> 01:43:33.817
with respect to understanding, uh, the
trout population. His experience

01:43:33.850 --> 01:43:38.616
was mostly up in Canada and Alaska
with rainbow trout and, and other

01:43:38.649 --> 01:43:43.635
species of trout. So, uh, a and his
name was Josh Corman. I apologize for

01:43:43.668 --> 01:43:47.357
not remembering that earlier, Josh
Corman was also instrumental and, and

01:43:47.390 --> 01:43:51.786
Josh is still working in the canyon
now. He works a lot with Mike Yard and

01:43:51.819 --> 01:43:56.147
they've done a absolutely marvelous
job of, of better understanding the

01:43:56.180 --> 01:43:59.916
population of rainbow trout,
especially rainbow trout, but brown trout as

01:43:59.949 --> 01:44:04.156
well in the Grand Canyon, how those
populations function, how they spawn

01:44:04.189 --> 01:44:08.595
the survival of the young, what
habitats they use, how they are affected

01:44:08.628 --> 01:44:13.737
by operation of Glen Canyon Dam. One
of the things that they found out is

01:44:13.770 --> 01:44:19.515
that, for example, uh, when, uh, the,
the, the rainbow trout in the Grand

01:44:19.548 --> 01:44:23.756
Canyon is a, is actually a late winter
spawner, they spawn in about

01:44:23.789 --> 01:44:28.906
January, February. And when they, and,
and their eggs will incubate for 60

01:44:28.939 --> 01:44:33.446
to maybe, maybe as much as well for 40
or maybe 60 days, something like

01:44:33.479 --> 01:44:38.666
that. When they hatch, when they
emerge, they will go to the near

01:44:38.699 --> 01:44:44.717
shoreline areas a as fry. So when
they're very, very young, they're

01:44:44.750 --> 01:44:49.796
looking for shallow sheltered areas.
So they will go into the shorelines

01:44:49.829 --> 01:44:55.366
in that lease ferry area and go to
about the shallow area. If you are

01:44:55.399 --> 01:45:00.305
running a fluctuating flow scenario,
you're going to strand those

01:45:00.338 --> 01:45:05.289
individuals, right? Because they're in
very, very low, very shallow water.

01:45:05.979 --> 01:45:07.979
Now, as they get older, they go from these low angle shorelines to the

01:45:11.168 --> 01:45:15.857
more high angle shorelines to more
rocky steeper shorelines. So

01:45:15.890 --> 01:45:21.095
understanding that of course, enables
you to better understand not just

01:45:21.128 --> 01:45:28.046
how the population survived but
perhaps potential um management flows for

01:45:28.079 --> 01:45:34.446
regulating those populations. So as a
result of that, the concept of

01:45:34.479 --> 01:45:39.546
trough management flows came about
that you can regulate the population to

01:45:39.579 --> 01:45:45.336
a certain degree if you want to by
basically raising flows to a certain

01:45:45.369 --> 01:45:51.987
level, say 15,000 cubic feet per
second in that January. Well, in about,

01:45:52.020 --> 01:45:58.906
in about that March, April period and
have those young fish go up on those

01:45:58.939 --> 01:46:04.706
shallow areas in le ferry, then drop
the water on them quite suddenly and

01:46:04.739 --> 01:46:09.666
you strand them, you regulate the
population that way by not having to do

01:46:09.699 --> 01:46:13.916
any mechanical removal by not having
to intercept the fish in the pet a

01:46:13.949 --> 01:46:19.015
badger reach by maybe not having to
worry about the fish moving downstream

01:46:19.048 --> 01:46:22.956
to the LCR because there, there is a
certain degree of density dependence

01:46:22.989 --> 01:46:26.626
that takes place with these
populations. Whereas if you have too many

01:46:26.659 --> 01:46:33.527
trout in the least ferry reach just by
common sense, the surplus of those

01:46:33.560 --> 01:46:37.555
fish are going to want to leave that
area and would move downstream. So

01:46:37.588 --> 01:46:41.756
that's been another option as an
alternative to mechanical removal is

01:46:41.789 --> 01:46:45.857
better understanding the population
than managing those populations to

01:46:45.890 --> 01:46:50.226
where they don't exceed their carrying
capacity for the system. Has anyone

01:46:50.259 --> 01:46:58.196
tried that option yet? Uh Yes. Um
Drought management flows have been

01:46:58.229 --> 01:47:05.119
implemented on an experimental basis.
They have worked to a certain degree.

01:47:05.930 --> 01:47:07.930
But again, there are these little twists of fate, so to speak, where um,

01:47:14.689 --> 01:47:20.726
the, the a, a big part of the uh trout
population in Grand Canyon least

01:47:20.759 --> 01:47:25.345
ferry reach was in fact, not
necessarily spawning in those shallow areas.

01:47:25.378 --> 01:47:28.925
They're spawning to more toward the
middle of the channel. You still have

01:47:28.958 --> 01:47:33.967
some of those young fish coming up
that combined with the with warmer

01:47:34.000 --> 01:47:40.756
releases of out of the dam have also
expanded the, the window of spawning.

01:47:40.789 --> 01:47:46.036
So we have those young of different
ages now being more occurring more

01:47:46.069 --> 01:47:51.046
over longer periods of time. So those
have been effective at some times

01:47:51.079 --> 01:47:56.206
and perhaps not so much at others
because of these nuances having to do

01:47:56.239 --> 01:48:01.076
with spawning. What we think is
happening now that Brown Trout Management

01:48:01.109 --> 01:48:06.067
team, what we concluded from that is
that one of the possibilities is that

01:48:06.100 --> 01:48:08.946
, um,

01:48:08.979 --> 01:48:14.055
that, that there's competition for uh
spawning areas between rainbow trout

01:48:14.088 --> 01:48:19.147
and brown trout to where you could
have 11 species spawning on top of the

01:48:19.180 --> 01:48:23.046
other because brown trout are fall
spawners. And so there's almost an

01:48:23.079 --> 01:48:26.696
overlap in the spawning now between
brown trout that spawned in October,

01:48:26.729 --> 01:48:31.446
November, December, even in January
and rainbow trout that are spawning in

01:48:31.479 --> 01:48:36.246
maybe even late December, January,
February. So you have a little bit of

01:48:36.279 --> 01:48:40.675
that competition, maybe taking place
as well. So these are again, the

01:48:40.708 --> 01:48:44.246
things that are still being looked at
to, to better know how to manage

01:48:44.279 --> 01:48:52.076
that system. But I think the the
important message here is that um if you

01:48:52.109 --> 01:48:56.616
understand the life history of the
species, it may not be a direct

01:48:56.649 --> 01:49:01.916
sledgehammer. That's the solution. You
may be able to find out nuances

01:49:01.949 --> 01:49:05.756
about the life history. And that's
what people like Carl Walters and Bill

01:49:05.789 --> 01:49:13.527
Pine enable us to understand. Now, um
There have been of course, other

01:49:13.560 --> 01:49:18.666
scientists that have been very
instrumental, Jack Schmidt I think is one

01:49:18.699 --> 01:49:24.857
whose name is associated. In fact,
almost with a Grand Canyon. Jack was at

01:49:24.890 --> 01:49:28.817
the front of better understanding this
concept of sediment distribution to

01:49:28.850 --> 01:49:32.746
the system, the concept of beach
habitat building flows and high flow

01:49:32.779 --> 01:49:36.237
experiments. He was right in the
middle. I remember I was down there in

01:49:36.270 --> 01:49:42.237
1996 during the that control flood and
I was uh doing fisheries work down

01:49:42.270 --> 01:49:46.416
uh just downstream of the little
Colorado River. He came by and he was

01:49:46.449 --> 01:49:49.196
doing some of the research he was
doing, of course, on sediment. They were

01:49:49.229 --> 01:49:54.036
tracing the dye as it was, they, they
had introduced dye into the water

01:49:54.069 --> 01:49:57.756
and they wanted to understand the
kinematic waves through the system. So

01:49:57.789 --> 01:50:01.187
Jack of course, has been instrumental
and he's many, had many graduate

01:50:01.220 --> 01:50:05.746
students down there. Paul Grahams is
one of those. Paul is now a member of

01:50:05.779 --> 01:50:09.937
the staff of the Grand Canyon
Monitoring Research Center. So he carries

01:50:09.970 --> 01:50:16.206
forth that so called flag of, of
sediment, you know, geom morphologies

01:50:16.239 --> 01:50:21.576
that are in the Grand Canyon. Um

01:50:21.609 --> 01:50:27.737
and most recently and probably most
significantly, uh a gentleman named

01:50:27.770 --> 01:50:34.996
Charles Yuli, who is a graduate of
Columbia University. And Oxford Charles

01:50:35.029 --> 01:50:40.226
joined the Grand Canyon Monitoring
Research Center in 2000, about 2010,

01:50:40.259 --> 01:50:45.586
2011. They hadn't been there very
long, but he his back, he has a very,

01:50:45.619 --> 01:50:53.166
very strong background in quantitative
ecology and he has a an uh an

01:50:53.199 --> 01:51:00.857
incredible background in uh ecosystem
uh models and ecosystem design and

01:51:00.890 --> 01:51:06.067
has the ability to be able to bring
together complex interactions among

01:51:06.100 --> 01:51:11.527
different species of organisms and has
focused some of his focus has been

01:51:11.560 --> 01:51:15.515
on Humpback Chub where he has helped
us to really understand that

01:51:15.548 --> 01:51:19.376
relationship between the mains stem
Colorado River and the Little Colorado

01:51:19.409 --> 01:51:24.226
River. And how Humpback Chub are using
that system. Charles was

01:51:24.259 --> 01:51:31.095
instrumental in doing the evaluation
of the alternatives of the 2016 EIS

01:51:31.128 --> 01:51:36.786
he coordinate uh across the different
disciplines, all the data that was

01:51:36.819 --> 01:51:41.476
available from hydrology to sediment
to humpback job, to trout, to repair

01:51:41.509 --> 01:51:45.626
and habitat, to recreation,
everything. He's the one that coordinate all

01:51:45.659 --> 01:51:50.696
that work. He has been a significant,
uh I think scientist in the Grand

01:51:50.729 --> 01:51:56.515
Canyon, especially most recently. Um
Larry Stevens. Of course, what can

01:51:56.548 --> 01:52:00.616
you say about Larry Stevens? Larry
Stevens is just the person who has just

01:52:00.649 --> 01:52:07.515
been there all the time. His, his uh
knowledge, his areas of expertise. In

01:52:07.548 --> 01:52:12.925
fact, um, go across virtually every
discipline you can think of in the

01:52:12.958 --> 01:52:17.506
Grand Canyon. Larry is always out
there. Larry doesn't do trips down the

01:52:17.539 --> 01:52:23.845
river to study one thing, Larry when
he's down there is looking at fish,

01:52:23.878 --> 01:52:27.076
he's looking at lizards, he's looking
at insects, he's looking at

01:52:27.109 --> 01:52:31.546
virtually everything around him. One
of the most incredible ecologists I

01:52:31.579 --> 01:52:35.996
think that, that I can think of
anyway. His knowledge is almost

01:52:36.029 --> 01:52:40.737
insurmountable in terms of
understanding the, the Grand Canyon. I think

01:52:40.770 --> 01:52:44.946
another one who goes back, in fact,
predates me certainly and predates

01:52:44.979 --> 01:52:48.916
many, many biologists in the Grand
Canyon. He was one of the first to

01:52:48.949 --> 01:52:52.187
conduct fish surveys through the Grand
Canyon and that's Steve Carruthers

01:52:52.220 --> 01:53:00.006
, Steve Carruthers, um, uh, was the
manager of the museum in Northern

01:53:00.039 --> 01:53:04.956
Arizona, which is right there in
Flagstaff and he, uh, started the company

01:53:04.989 --> 01:53:11.996
SWC A back in the, in the seventies
and I, I happened to, to run, well, I

01:53:12.029 --> 01:53:17.476
, my relationship with Steve was that
we were both bidding on that

01:53:17.509 --> 01:53:22.036
humpback job. Life, history, ecology
work. The reclamation issued back in

01:53:22.069 --> 01:53:28.147
the, in the late 19 eighties and, and
I won the contract and he did not.

01:53:28.180 --> 01:53:31.756
And so he finally came up to me one
day and he said, you know, I'm tired

01:53:31.789 --> 01:53:35.546
of you and I competing against each
other. We should join forces. And

01:53:35.579 --> 01:53:39.885
that's been a wonderful relationship
that I've had with Steve since he's a

01:53:39.918 --> 01:53:44.857
, if you want to know about birds in
the Grand Canyon or reptiles in the

01:53:44.890 --> 01:53:48.277
Grand Canyon, Steve Carruthers is one
of the more knowledgeable. Certainly

01:53:48.310 --> 01:53:54.876
, I'm sure I'm, I'm leaving certain
scientists out, but those are the ones

01:53:54.909 --> 01:53:59.987
that come to me at this time. How
about key reports or studies that you

01:54:00.020 --> 01:54:04.107
want to highlight is particularly
important that have retained their value

01:54:04.140 --> 01:54:12.140
over time? Yeah. Um Well, certainly,
um

01:54:12.168 --> 01:54:20.168
the uh the final environmental impact
statement of 1996 is, is pivotal. Um

01:54:20.819 --> 01:54:25.967
because of that was the first, there,
there was never ne a compliance done

01:54:26.000 --> 01:54:32.476
on Glen Canyon Dam because it was
built way before NE A and so that was

01:54:32.509 --> 01:54:39.076
the first effort to try to consolidate
all that information. Um

01:54:39.109 --> 01:54:46.467
The uh the 2016, the most recent LT MP
I SI think is also a good archival

01:54:46.500 --> 01:54:53.467
document for many of the things that
have taken place. There are four

01:54:53.500 --> 01:54:57.746
reviews from the National Academy of
Sciences that I think people, people

01:54:57.779 --> 01:55:01.805
sometimes overlook in terms of going
back and looking at the history of

01:55:01.838 --> 01:55:05.595
the Grand Canyon. And I think those
are significant because it really

01:55:05.628 --> 01:55:11.777
shows this, this transition uh and
evolution of thinking by scientists in

01:55:11.810 --> 01:55:16.376
the Grand Canyon, as I mentioned
earlier, uh the first review because it

01:55:16.409 --> 01:55:21.527
was right after the 8384 high flows,
the natural high flows through. There

01:55:21.560 --> 01:55:27.015
was of course historic snowfall in the
upper Colorado River Basin. Uh I

01:55:27.048 --> 01:55:32.256
remember doing cataract at about 75
80,000 CFS. And it was a, it was a

01:55:32.289 --> 01:55:37.416
nightmare and of course, flows through
the Grand Canyon reached a peak of

01:55:37.449 --> 01:55:42.595
almost 90,000 CFS when everything was
being allowed to go downstream of

01:55:42.628 --> 01:55:47.326
the dam. And as a result of that, when
the National Academy of Sciences

01:55:47.359 --> 01:55:51.616
met, they said don't do any kind of
high flows in the Grand Canyon, right

01:55:51.649 --> 01:55:56.036
? Because that'll flush all the
sediment downstream into lake mead. Well,

01:55:56.069 --> 01:56:00.206
of course, subsequent reviews from the
National Academy of Sciences said,

01:56:00.239 --> 01:56:03.607
no, that's not really true. And again,
Jack Schmidt, I think was

01:56:03.640 --> 01:56:09.796
instrumental in bringing that back to
some common sense management policy

01:56:09.829 --> 01:56:13.777
that could be put in place. And so now
we have it's not policy. It's

01:56:13.810 --> 01:56:17.897
experiments. Now we have the high flow
experiments that are in fact

01:56:17.930 --> 01:56:23.656
showing that that is one way to
conserve sediment in the Grand Canyon. Um

01:56:23.689 --> 01:56:29.786
There are of course a collection of
reports and published manuscripts

01:56:29.819 --> 01:56:34.817
having to do with the Grand Canyon,
wonderful pieces of work by many, many

01:56:34.850 --> 01:56:40.976
scientists. Um The one that the one
that, that I, that I was associated

01:56:41.009 --> 01:56:49.009
with that I'm most proud of is uh 1999
publication in bioscience. Uh that

01:56:49.699 --> 01:56:55.406
I did with uh Jack Schmidt was the
lead author. Uh Bob Webb was involved

01:56:55.439 --> 01:57:00.126
in it, Dick Marzo, Larry Stevens and
myself. It was, it was the result of

01:57:00.159 --> 01:57:04.967
a brainchild that took place in San
Francisco. We were, we were at the uh

01:57:05.000 --> 01:57:11.246
Geophysical Union meeting in San
Francisco sitting uh in the, in the

01:57:11.279 --> 01:57:18.187
lounge in between sessions. And Jack
had asked the five of us to get

01:57:18.220 --> 01:57:25.416
together. And he said, uh gentlemen,
we should, we should document what

01:57:25.449 --> 01:57:28.756
we're learning in the Grand Canyon.
This is before the concept of adaptive

01:57:28.789 --> 01:57:32.237
management. This is before any of that
had ever come together. This is

01:57:32.270 --> 01:57:38.107
before Carl Walters or anybody. And he
said, what do we know and what we,

01:57:38.140 --> 01:57:42.217
what have we learned? And we went
through uh I, I wish I had recorded it

01:57:42.250 --> 01:57:47.576
because it was a wonderful
conversation with um who I considered the top

01:57:47.609 --> 01:57:51.737
scientists probably that were
involved, you know, Dick Marzo was at that

01:57:51.770 --> 01:57:57.626
time with the uh US Geological Survey
out of Reston, Virginia. He was one

01:57:57.659 --> 01:58:02.416
of the main science coordinators for
us, GS Bob Webb was out of us GS out

01:58:02.449 --> 01:58:07.996
of Tucson, one of the noted
authorities on Whitewater Rapids and had done

01:58:08.029 --> 01:58:12.226
a lot of work in the Grand Canyon on
lava falls on lava rapid and so on.

01:58:12.259 --> 01:58:15.425
And of course, Larry Stevens was
involved in that as well and we sat

01:58:15.458 --> 01:58:21.967
around and talked about what it is
that was happening in the Grand Canyon

01:58:22.000 --> 01:58:26.156
and what was possible in terms of
science. And so it was called Science

01:58:26.189 --> 01:58:30.726
and Values in the Grand Canyon. That
was the, the title we came up with

01:58:30.759 --> 01:58:37.925
the conclusions I thought were
remarkable for that time, given our

01:58:37.958 --> 01:58:42.916
fundamentally feeble understanding of
the way the system worked, but we

01:58:42.949 --> 01:58:46.135
made observations over what we saw.
And one of the things that we

01:58:46.168 --> 01:58:50.937
concluded was was this concept of what
we referred to as the intractable

01:58:50.970 --> 01:58:57.476
dilemma where um we realized and
recognized that there was no single

01:58:57.509 --> 01:59:03.107
management action that could,

01:59:03.140 --> 01:59:10.345
that could simultaneously benefit all
resources. You couldn't have one

01:59:10.378 --> 01:59:15.885
Glen Canyon Dam operations that would
be best for sand and best for

01:59:15.918 --> 01:59:19.666
Humpback chub and best for repairing
habitat and recreation and everything

01:59:19.699 --> 01:59:24.487
else. It didn't work that way. You of
course, had different conditions

01:59:24.520 --> 01:59:28.696
that were available at different times
of the year. And so you basically,

01:59:28.729 --> 01:59:33.416
you managed according to that. And,
and so what that did is it

01:59:33.449 --> 01:59:38.336
fundamentally opened the door
beautifully for adaptive management whereby

01:59:38.369 --> 01:59:42.305
you recognize that you realize that
and you say, OK, what we have to do

01:59:42.338 --> 01:59:46.256
then is implement a series of, of
experiments over hypotheses. And then

01:59:46.289 --> 01:59:49.817
you evaluate those over time, they
work sometimes they don't work. Other

01:59:49.850 --> 01:59:55.717
times you benefit some resources,
sometimes not other times. So that, that

01:59:55.750 --> 02:00:00.265
uh val science and values in the Grand
Canyon and Bioscience 1999 was I

02:00:00.298 --> 02:00:04.777
think a, a landmark paper.

02:00:04.810 --> 02:00:11.116
Um Thanks again to Jack, I think
largely to Jack Schmidt on that one. Um

02:00:11.149 --> 02:00:14.786
There were a number of other papers of
course, that were published by Lou

02:00:14.819 --> 02:00:19.536
Coggins, Carl Walters on Humpback chub
populations. It was the first

02:00:19.569 --> 02:00:24.256
opportunity we had to really bring
together the, the life history and

02:00:24.289 --> 02:00:29.076
ecology. The work that I had done was
mostly in a large report. They, I

02:00:29.109 --> 02:00:32.876
think, uh you know, very well brought
that information together and

02:00:32.909 --> 02:00:40.206
published it. Um did an excellent job
of that. Um Then, and there and

02:00:40.239 --> 02:00:44.456
those papers are in various journals
uh that you can find. And then most

02:00:44.489 --> 02:00:50.296
recently Charles Yuli published a
paper about now uh about six or seven

02:00:50.329 --> 02:00:55.506
years ago and, and it is uh it, it's
entitled Something Like Growth and

02:00:55.539 --> 02:01:00.366
Survival of Humpback Chub in the Grand
Canyon. And he, and he has a, this

02:01:00.399 --> 02:01:06.187
is this is, this is how scientists
think wonderfully. He has a lot of

02:01:06.220 --> 02:01:14.220
little uh icons of fish as part of his
models in that manuscript showing

02:01:14.378 --> 02:01:19.366
how Humpback Chub come from the main
stem into the LCR spawn and then

02:01:19.399 --> 02:01:23.536
their little babies come drifting out
or move into the main stem and then

02:01:23.569 --> 02:01:26.555
grow up and then turn around and some
of them come back and some of them

02:01:26.588 --> 02:01:30.737
don't. And then there's a concept of
skipped spawning where they don't

02:01:30.770 --> 02:01:36.147
spawn every year, they may skip a
year. And so he very nicely

02:01:36.180 --> 02:01:40.496
characterized that in the paper and,
and it's by Charles Yuli. I think

02:01:40.529 --> 02:01:48.529
it's a wonderful piece of work. How do
you spell Ky Ac Kul, IC Charles

02:01:48.930 --> 02:01:56.027
Yuli. And that was co-authored by, uh,
Mike Yard, Randy Van Habe. And, um

02:01:56.060 --> 02:01:59.906
oh my goodness. I uh I can't remember
who the other author is. We'll look

02:01:59.939 --> 02:02:04.067
it up. Yeah, but that was, that's a,
that's a very good paper, more, more

02:02:04.100 --> 02:02:12.100
recent type of paper. Um Jack, of
course, Schmidt did some uh landmark

02:02:13.298 --> 02:02:19.345
pieces of work that I think can be
found under his name relative to Grand

02:02:19.378 --> 02:02:22.976
Canyon. Um

02:02:23.009 --> 02:02:26.885
Those are the ones that come, I think
to mind at, at this time, Graham.

02:02:26.918 --> 02:02:34.166
Great, thanks. Well, how about a
couple of big picture questions? What do

02:02:34.199 --> 02:02:42.006
you think is the value of adaptive
management in trying to manage complex

02:02:42.039 --> 02:02:49.456
resources in an environment that we
can't predict or control?

02:02:49.489 --> 02:02:56.737
Yeah. And, and that's uh that's
probably the, the, you know, $50 million

02:02:56.770 --> 02:03:04.770
question, I think for, for many
systems, um The, the Grand Canyon system

02:03:05.000 --> 02:03:10.647
is somewhat similar to other river
basin programs across the Western

02:03:10.680 --> 02:03:18.680
United States in that there are most
river basin programs have dams or

02:03:19.600 --> 02:03:24.006
water diversions or whatever that have
fundamentally altered the basic

02:03:24.039 --> 02:03:29.156
structure. And function of the
ecosystem ecosystems that in the case of

02:03:29.189 --> 02:03:33.296
the Colorado River were probably in
place although dynamic, maybe over a

02:03:33.329 --> 02:03:39.765
period of 3 to 4 million years. And
yes, in the Grand Canyon probably

02:03:39.798 --> 02:03:44.777
about a million years ago or so, there
were uh it, it was a very

02:03:44.810 --> 02:03:50.717
seismically active area at the time
that the plateau was rising. There is

02:03:50.750 --> 02:03:55.126
very strong evidence that there were
lava flows that dammed the Colorado

02:03:55.159 --> 02:04:00.717
River in the Grand Canyon and those
dams probably lasted quite some time.

02:04:00.750 --> 02:04:04.595
Although the releases were not
Hypolite coal releases, like we see today

02:04:04.628 --> 02:04:10.336
, they probably were overflow or
topping over the top of those lava dams

02:04:10.369 --> 02:04:13.777
until they eventually eroded over a
period of time. Some of those

02:04:13.810 --> 02:04:17.126
presumably could have lasted about
1000 years, perhaps, perhaps a little

02:04:17.159 --> 02:04:25.159
less. Um so, but, but fundamentally, I
you can, despite the dynamics that

02:04:26.329 --> 02:04:31.237
you see over say a million years or a
3 to 4 million year period, you

02:04:31.270 --> 02:04:36.095
still recognize that there was a
dynamic system that was there before

02:04:36.128 --> 02:04:40.956
there were any uh any um

02:04:40.989 --> 02:04:47.187
any of man's influences such as dams
such as water diversions, such as

02:04:47.220 --> 02:04:52.976
depletion of sediment and so on

02:04:53.009 --> 02:04:58.626
when one considers those kinds of
effects.

02:04:58.659 --> 02:05:04.616
The first, the first thing to
understand is that it is unlikely that that

02:05:04.649 --> 02:05:09.187
so-called historical system, whatever
that used to look like. Pre Preman

02:05:09.220 --> 02:05:16.256
say, it's unlikely that that would
ever be restored to what it was. And so

02:05:16.289 --> 02:05:21.546
you have to, you have to work with an
altered system. It is also unlikely

02:05:21.579 --> 02:05:25.885
that one can restore the the function,
the structure and function of the

02:05:25.918 --> 02:05:30.217
components of that system. The way the
river used to work, the big floods

02:05:30.250 --> 02:05:35.175
in the spring time, the high
temperatures, et cetera, the absence of of

02:05:35.208 --> 02:05:43.208
alien fish. And so um so the the
problems are so, so the problem becomes

02:05:43.588 --> 02:05:48.076
first understanding the way the system
works in its current state, the

02:05:48.109 --> 02:05:52.506
dynamics of that contemporary river
system.

02:05:52.539 --> 02:05:57.555
And part of that, of course is trying
to better explain how some

02:05:57.588 --> 02:06:01.496
components of that system might work
that are in scientific terms,

02:06:01.529 --> 02:06:09.529
expressed as hypotheses. And so it is,
it is in fact the almost the ideal

02:06:09.649 --> 02:06:15.616
setting for adaptive management
whereby you try to explain a particular

02:06:15.649 --> 02:06:19.027
problem or a particular issue having
to do with the Grand Canyon or

02:06:19.060 --> 02:06:23.175
operation of Grand Canyon Dam, you
establish a hypothesis and then you

02:06:23.208 --> 02:06:27.647
test that hypothesis in different
ways. You realize that when you do test

02:06:27.680 --> 02:06:30.817
it like high flow experiments, for
example, you don't quite get it right.

02:06:30.850 --> 02:06:35.437
The first time the first high flow
experiment was 1996 we went for 10 or

02:06:35.470 --> 02:06:39.336
12 days. I can't remember how long it
was and most of the sediment moved

02:06:39.369 --> 02:06:43.555
in about the first two or three days.
So we learn from that, we learn that

02:06:43.588 --> 02:06:46.897
those don't need to be as long. So
that was part of the cycle of adaptive

02:06:46.930 --> 02:06:52.116
management. Uh It's true of virtually
every resource in the Grand Canyon

02:06:52.149 --> 02:06:57.107
that you have to understand that. So
adaptive management in, in, in, in

02:06:57.140 --> 02:07:02.996
and of itself as a concept is probably
well suited to something like like

02:07:03.029 --> 02:07:09.397
Grand Canyon to, to be implemented in
that, in that system. Now, what Carl

02:07:09.430 --> 02:07:13.726
Walters also taught us though was what
we talked about earlier. Those

02:07:13.759 --> 02:07:17.906
unexpected surprises that nature may
throw on you. The condition

02:07:17.939 --> 02:07:24.126
dependency where you have times when
you cannot implement an experiment

02:07:24.159 --> 02:07:28.836
because there's not enough water
available to do it or the experiment goes

02:07:28.869 --> 02:07:32.956
awry because the temperatures weren't
what you expected from the river.

02:07:32.989 --> 02:07:38.175
Again, you're basically doing
experimentation in a large open laboratory

02:07:38.208 --> 02:07:43.246
with no control whatsoever except for
perhaps a large spigot call Glen

02:07:43.279 --> 02:07:51.279
Canyon Dam. And so um the the to me,
the most informative part of it

02:07:53.029 --> 02:07:58.906
though is to be able to implement
adaptive management and then perhaps

02:07:58.939 --> 02:08:03.425
even remove yourself from the program
as, as I have and not that I've

02:08:03.458 --> 02:08:07.576
removed myself, but I, I'm not as
involved as I was. And then look at it

02:08:07.609 --> 02:08:13.397
from the outside in, in a really
objective way and look at what it has

02:08:13.430 --> 02:08:19.946
worked and what hasn't worked. And I
think by and large um aspects of what

02:08:19.979 --> 02:08:25.756
has have been put in place, have
worked and aspects of it have not worked

02:08:25.789 --> 02:08:33.616
in some cases. Um Well, for example,
the, the, the concept of um when we

02:08:33.649 --> 02:08:39.226
first started looking at mechanical
non fish control, we thought, OK, we

02:08:39.259 --> 02:08:42.296
can, we can go in there and put
electro fishing boats in the river and

02:08:42.329 --> 02:08:46.836
take out a lot of trout and that'll
solve the problem. Well, not quite

02:08:46.869 --> 02:08:51.826
because you had this invasion, this re
invasion of those areas. Uh Another

02:08:51.859 --> 02:08:55.487
example is perhaps uh high flow
experiments where you're trying to

02:08:55.520 --> 02:08:59.305
preserve sand and sediment. You take
advantage of when that sediment is

02:08:59.338 --> 02:09:04.626
most available in the fall. But now
perhaps you're scouring the food base.

02:09:04.659 --> 02:09:08.536
And so you have to understand that
every one of those actions that you're

02:09:08.569 --> 02:09:13.595
implementing as, as an experiment has
some kind of reaction perhaps to

02:09:13.628 --> 02:09:18.647
other resources. So again, that's
something that Carl Walters cautioned us

02:09:18.680 --> 02:09:22.765
about that management, that
experimentation, you have to go through

02:09:22.798 --> 02:09:27.467
experimentation first before you
implement policy. Before you put that as

02:09:27.500 --> 02:09:32.876
part of your normal operation, you
have to evaluate it first. What many of

02:09:32.909 --> 02:09:36.546
us did not understand and certainly
many managers and administrators and

02:09:36.579 --> 02:09:42.996
even today don't understand is how
long that takes to do that. I mean,

02:09:43.029 --> 02:09:48.336
we've had a science program in the
Grand Canyon since about 1985 with G Ce

02:09:48.369 --> 02:09:53.796
s with Dave Wagner. That's a long time
that you know, that's 30 some odd

02:09:53.829 --> 02:09:58.187
years of experimentation in the Grand
Canyon. And of course, managers

02:09:58.220 --> 02:10:01.305
always say, how long is this gonna
take you? When are you going to give us

02:10:01.338 --> 02:10:08.067
the answer. Well, there is no
particular answer. It really, it really

02:10:08.100 --> 02:10:14.496
speaks to the need for ongoing
involvement, an ongoing understanding of

02:10:14.529 --> 02:10:19.967
what's happening in the system and the
ongoing dynamics. So that to me is

02:10:20.000 --> 02:10:25.826
the most valuable part is this
retrospective opportunity to look back on

02:10:25.859 --> 02:10:31.706
it and see what worked, what didn't
work and what surprises we had. And

02:10:31.739 --> 02:10:38.647
it's that last one that's often the
largest effect of any of those.

02:10:38.680 --> 02:10:41.376
Well, that's a,

02:10:41.409 --> 02:10:48.095
an articulate defense of the value of
the program over time. Um Yeah, it's

02:10:48.128 --> 02:10:53.777
been 30 I think, 38 years since the
launching of G ce S one that came up,

02:10:53.810 --> 02:11:01.810
started in 1982 almost four decades
and 25 years since um the launching of

02:11:01.869 --> 02:11:08.015
the Glen Canyon Dam Adaptive
Management Program proper.

02:11:08.048 --> 02:11:13.616
It's pretty expensive program. We have
learned a lot. Do you anticipate

02:11:13.649 --> 02:11:19.107
that there will be some point in the
future in which the program is, we've

02:11:19.140 --> 02:11:22.906
learned enough that we don't really
need the program anymore? Or is the

02:11:22.939 --> 02:11:27.726
constant evolution and accretion of
knowledge so valuable that it should

02:11:27.759 --> 02:11:32.015
be continued, at least for the
foreseeable future in your opinion. Well,

02:11:32.048 --> 02:11:36.476
unfortunately, the continuance of that
program is not under our control,

02:11:36.509 --> 02:11:42.006
of course, but I would certainly hope
that that program continue. And the

02:11:42.039 --> 02:11:47.687
reason is because, um it's not for
science, it's not for the sake of

02:11:47.720 --> 02:11:52.425
science alone. It is for the sake of
better understanding how to manage

02:11:52.458 --> 02:11:57.006
one of the most valuable resources we
have in North America and society

02:11:57.039 --> 02:12:03.506
has made that decision that it's
important to maintain the Grand Canyon as

02:12:03.539 --> 02:12:08.095
well as we can and maintain all the
resources within the Grand Canyon when

02:12:08.128 --> 02:12:14.487
it is a societal decision and it is a
s a societal value. I think it does

02:12:14.520 --> 02:12:20.576
rise to the level of justifying an
ongoing funding of the program in its

02:12:20.609 --> 02:12:28.609
current state. It is a um it is a
federal advisory committee so it's under

02:12:29.859 --> 02:12:35.036
the direct authority of the Secretary
of the Interior. I hope it stays

02:12:35.069 --> 02:12:40.967
that way because it, it certainly, I
think has um eliminated a lot of the

02:12:41.000 --> 02:12:46.656
complexity, especially for funding the
program. Now, whether that can be

02:12:46.689 --> 02:12:52.635
part back, some, I think only managers
can make that decision. Uh Again,

02:12:52.668 --> 02:12:58.345
the the the role of science in the
process is gathering information in an

02:12:58.378 --> 02:13:04.217
in an objective manner in order to
give that information for managers to

02:13:04.250 --> 02:13:08.357
make informed decisions and for
administrators to facilitate those

02:13:08.390 --> 02:13:12.756
decisions and provide the logistics
for those being done. I think that's

02:13:12.789 --> 02:13:16.265
important. I think those roles are
necessary in a system like the Grand

02:13:16.298 --> 02:13:21.226
Canyon. And again, not for the sake of
science, but really for the sake of

02:13:21.259 --> 02:13:24.996
the resources in the Grand Canyon, not
just in the Grand Canyon, but

02:13:25.029 --> 02:13:28.217
downstream as well. Because that water
that's delivered through the system

02:13:28.250 --> 02:13:33.446
is also important to the downstream
states, Nevada, California, and

02:13:33.479 --> 02:13:40.496
Arizona as well. As it, as it goes
downstream. So I, I see. And I'm hoping

02:13:40.529 --> 02:13:47.987
that the program continues in some
form because I think it's necessary um

02:13:48.020 --> 02:13:55.256
to do so if one were to um speculate a
little bit on what might happen, if

02:13:55.289 --> 02:14:02.015
the program would go away. For one
thing we've learned from programs like

02:14:02.048 --> 02:14:06.996
the Grand Canyon program, like the
upper Colorado River recovery program,

02:14:07.029 --> 02:14:12.515
like the San Juan River recovery
implementation program, like the lower

02:14:12.548 --> 02:14:18.076
Colorado river MS CP. We've learned
that those programs have certainly

02:14:18.109 --> 02:14:24.666
brought together all of the interest
in the system. Many millions of

02:14:24.699 --> 02:14:29.286
people rely on these rivers for
delivery of water for recreation, for many

02:14:29.319 --> 02:14:35.237
other values. Those are those programs
are important to maintain because I

02:14:35.270 --> 02:14:40.616
, I do remember before, for example,
the Upper Colorado River Basin

02:14:40.649 --> 02:14:48.277
program, I do remember uh what were
then almost termed water wars where

02:14:48.310 --> 02:14:52.206
there was some uncertainty about how
to best manage the water, who owned

02:14:52.239 --> 02:14:57.616
the water, how it was to be
transferred and passed through the system. Um

02:14:57.649 --> 02:15:02.506
People like Tom Pitts who was a water
coordinator in the upper Colorado

02:15:02.539 --> 02:15:06.765
River basin came up with many concepts
as to how to do this. And one of

02:15:06.798 --> 02:15:10.726
the ideas he came up with was to
establish a recovery implementation

02:15:10.759 --> 02:15:16.967
program which was to enable water
users to get together and talk about how

02:15:17.000 --> 02:15:19.737
to best manage

02:15:19.770 --> 02:15:26.156
water resources in concert with
natural resources. And so I am hoping that

02:15:26.189 --> 02:15:29.826
this program does continue

02:15:29.859 --> 02:15:37.217
last question. What advice would you
have for people coming newly into the

02:15:37.250 --> 02:15:43.937
program? Some young post doc who gets
his, his or her first research grant

02:15:43.970 --> 02:15:49.067
or somebody a stakeholder that gets uh
placed on the adaptive management

02:15:49.100 --> 02:15:52.126
work group or technical work group.
What advice would you have for them

02:15:52.159 --> 02:16:00.095
about how to be uh successful in
advancing the program,

02:16:00.128 --> 02:16:07.116
patience and humility, not necessarily
in that order.

02:16:07.149 --> 02:16:09.946
Um

02:16:09.979 --> 02:16:16.015
The uh the there are the recognition
that there have been many people

02:16:16.048 --> 02:16:22.366
before them working to the best of
their ability to try to put a program

02:16:22.399 --> 02:16:27.675
in place. The best man, the best
balances, water management and protection

02:16:27.708 --> 02:16:35.708
of resources. That's important, the
understanding of roles, especially

02:16:36.308 --> 02:16:42.105
those with scientific backgrounds to
understand that that the role of a

02:16:42.138 --> 02:16:46.626
scientist is in fact to provide
information by which others can make

02:16:46.659 --> 02:16:50.667
informed decisions. And that was one
of the big things that we talked

02:16:50.700 --> 02:16:54.546
about in that bioscience paper. I
mentioned earlier the role of science.

02:16:54.579 --> 02:17:00.456
That that's an important concept I
think because we make decisions on the

02:17:00.489 --> 02:17:05.785
basis of societal needs and societal
demands, not on the basis of what

02:17:05.818 --> 02:17:10.564
scientists think. However, the better
informed those decisions are the

02:17:10.597 --> 02:17:14.866
better off we're going to be. So I
think that that's important. The other

02:17:14.899 --> 02:17:18.385
part of it is humility and I certainly
learned that one the hard way

02:17:18.418 --> 02:17:23.855
because all of us uh as young phd s
think we pretty much know about all

02:17:23.888 --> 02:17:27.016
there is to know and just turn us
loose on the planet and we'll solve all

02:17:27.049 --> 02:17:33.194
the problems. Um You know, that that
is where people like Carl Walters and

02:17:33.227 --> 02:17:40.906
Bill Pine were so um so enigmatic
about being able to tell us how to

02:17:40.939 --> 02:17:45.906
better manage a system while being
patient with us and while being, you

02:17:45.939 --> 02:17:50.554
know, tutorial, more or less helping
us understand better how to, how to

02:17:50.587 --> 02:17:55.217
see things, how to view things. So I I
think, I think patients and

02:17:55.250 --> 02:17:59.946
humility are probably the best
guidance I could give to someone coming

02:17:59.979 --> 02:18:04.706
into the system. Uh be patient with
other stakeholders, especially those

02:18:04.739 --> 02:18:08.025
that have been in the program for some
time. They may be knowing things

02:18:08.058 --> 02:18:13.766
that may be a surprise. And yet at the
same time as a scientist, 1 may

02:18:13.799 --> 02:18:18.507
observe a new scientist may observe
that gosh, you guys recommended such

02:18:18.540 --> 02:18:22.587
and such back when and it didn't work,
did it? Well, again, that's part of

02:18:22.620 --> 02:18:26.257
patience. That's part of adaptive
management. No, it may have not worked.

02:18:26.290 --> 02:18:30.105
But let's look at it further, let's
let's do it better, let's figure out

02:18:30.138 --> 02:18:35.685
a way to do it better. Um And I see a
lot of new scientists coming into

02:18:35.718 --> 02:18:39.077
the program that I think are aware of
some of those fundamentals. I I

02:18:39.110 --> 02:18:44.626
certainly see people like Charles J
Kulick who has been very, very helpful

02:18:44.659 --> 02:18:48.327
and and understands that having worked
around the world, I think he's

02:18:48.360 --> 02:18:56.360
encountered these situations before.
But um the, the uh the GC Damp does a

02:18:56.500 --> 02:19:03.736
wonderful job of coordinating the
science. The twig technical work group

02:19:03.769 --> 02:19:08.226
of the GC Damp has done a wonderful
science of uh a wonderful job of

02:19:08.259 --> 02:19:12.657
helping to coordinate and, and
assimilate that information in a meaningful

02:19:12.690 --> 02:19:17.116
way. And they've been very good, I
think at issuing reports and reporting

02:19:17.149 --> 02:19:22.525
and, and giving scientists the
opportunity. Uh a good thing was to bring

02:19:22.558 --> 02:19:28.596
the US or the GCMRC under the US
Geological Survey because now if you go

02:19:28.629 --> 02:19:32.885
to the website, you will find all of
the reports. They're up to date.

02:19:32.918 --> 02:19:37.275
Everything is being archived in a very
good fashion. You don't have any

02:19:37.308 --> 02:19:40.577
trouble finding what people are doing.
You can see it right there. That's

02:19:40.610 --> 02:19:44.805
not true of all river basin programs.
This one is, is a wonderful example

02:19:44.838 --> 02:19:49.685
, is everything perfect. Of course
not. No, there are many things that

02:19:49.718 --> 02:19:54.946
need improvement within the, the GC
damp, but those are the kinds of

02:19:54.979 --> 02:19:58.467
things that you learn as you go and
you try to improve as, as best as

02:19:58.500 --> 02:20:06.366
possible. So, um yeah, like I said,
patience and humility.

02:20:06.399 --> 02:20:12.917
Well, thanks rich for um your meeting
with us today, for your wisdom and

02:20:12.950 --> 02:20:17.507
your openness and, and your lifetime
of research trying to advance these

02:20:17.540 --> 02:20:22.366
really important goals of balancing,
as you said, balancing societal needs

02:20:22.399 --> 02:20:28.217
with um with the health and resilience
of the ecosystems we depend on.

02:20:28.250 --> 02:20:31.866
Well, thank you. I appreciated uh you
asking me to do this interview and

02:20:31.899 --> 02:20:35.950
thoroughly enjoyed it. Thank you. Ok.