Section 1 Introduction ..................................................................... 3 1.1 Purpose...................................................................................................................... 3 1.2 Project Authority....................................................................................................... 3 1.3 Project Location ........................................................................................................ 4 1.4 Hydrologic and Hydraulic Methods.......................................................................... 4 1.5 Acknowledgments..................................................................................................... 5 1.6 Study Results ............................................................................................................ 5 Section 2 FEMA Forms .................................................................... 9 2.1 Study Documentation Abstract for FEMA submittals.............................................. 9 2.1.1 Date Study Accepted.......................................................................................... 9 2.1.2 Study Contractor ................................................................................................ 9 2.1.3 Local Technical Reviewer ................................................................................. 9 2.1.4 Reach Description.............................................................................................. 9 2.1.5 USGS Quad Sheets ............................................................................................ 9 2.1.6 Unique Conditions and Problems ...................................................................... 9 2.1.7 Coordination of Peak Discharges..................................................................... 10 2.2 FEMA Forms .......................................................................................................... 10 Section 3 Survey and Mapping Information................................. 10 3.1 Field Survey Information........................................................................................ 10 3.2 Mapping .................................................................................................................. 10 Section 4 Hydrology....................................................................... 10 4.1 Method Description ................................................................................................ 10 4.2 Parameter Estimation .............................................................................................. 11 4.2.1 Drainage Area .................................................................................................. 11 4.2.2 Watershed Work Map ...................................................................................... 11 4.2.3 Gage Data......................................................................................................... 11 4.2.4 Statistical Parameters ....................................................................................... 11 4.2.5 Precipitation ..................................................................................................... 11 4.2.6 Physical Parameters ......................................................................................... 12 4.3 Problems Encountered During the Study................................................................ 14 4.3.1 Special Problems and Solutions....................................................................... 14 4.3.2 Modeling Warning and Error Messages .......................................................... 14 4.4 Calibration............................................................................................................... 14 4.5 Final Results........................................................................................................ 14 4.5.1 Hydrologic Analysis Results........................................................................ 14 4.5.2 Verification results....................................................................................... 15 Section 5 Hydraulics ...................................................................... 16 5.1 Method Description ................................................................................................ 16 5.2 Work Study Maps ................................................................................................... 17 5.3 Parameter Estimation .............................................................................................. 18 5.3.1 Roughness Coefficients ................................................................................... 18 5.3.2 Expansion and Contraction Coefficients ......................................................... 18 5.4 Cross-Section Description ...................................................................................... 18 5.5 Modeling Consideration.......................................................................................... 18 5.5.1 Hydraulic Jump and Drop Analysis................................................................. 18 1 5.5.2. Bridges and Culverts....................................................................................... 18 5.5.3 Levees and Dikes ............................................................................................. 18 5.5.4 Island and Flow Splits...................................................................................... 19 5.5.5 Ineffective Flow Areas..................................................................................... 19 5.6 Floodway Modeling ................................................................................................ 19 5.7 Problems Encountered ............................................................................................ 19 5.7.1 Special Problems and Solutions....................................................................... 19 5.7.2 Model Warnings and Errors............................................................................. 19 5.8 Calibration............................................................................................................... 20 5.9 Final Results............................................................................................................ 20 5.9.1 Hydraulic Analysis Results.............................................................................. 20 5.9.2 Verification of Results ..................................................................................... 20 Section 6 Erosion and Sediment Transport................................. 21 Section 7 Draft FIS Report Data .................................................... 21 7.1 Summary of Discharges.......................................................................................... 21 7.2 Floodway Data ........................................................................................................ 21 7.3 Annotated Flood Insurance Rate Map .................................................................... 21 7.4 Flood Profiles.......................................................................................................... 21 Appendix A: References Appendix B: General Documentation and Correspondence Appendix C: Survey Field Notes Appendix D: Hydrologic Analysis, Supporting Documents Appendix E: Hydraulic Analysis, Supporting Documents Appendix F: Erosion Analysis, Supporting Documents Exhibit 1 Exhibit 2 Attached CD Casas Adobes TDN with supporting models and GIS data. List of Tables Table 4.1 Methods used for a HEC-HMS analysis Table 4.2. Physical Parameters for Sub-Basins Table 4.3. Physical Parameters for Reaches Table 4.4 Summary of sub-basin discharges. Table 4.5. Summary of 100-yr Peak Discharge Values Table 4.8. Comparison of peak discharge with regional regression equations. Table 7. Summary of Discharges List of Figures Figure 1.1 Casas Adobes Wash Watershed Map Figure 1.2 Study Limit of the Casas Adobes Wash Figure 1.3 Casas Adobes Wash Soil Classification Figure 5.1 The study areas for the three FLO-2D models. 2 Section 1 Introduction 1.1 Purpose This Technical Data notebook (TDN) has been prepared for the Casas Adobes Wash (CSA) located in Pima County, Arizona (Figure 1.1). The objective of the TDN is to provide discharges and floodplain limits along the CSA using better topographic, hydrologic, and hydraulic data. This TDN was prepared in accordance with the “Instructions for Organizing and Submitting Technical Documentation for Flood Studies” prepared by the Arizona Department of Water Resources, Flood Mitigation Section (Arizona State Standard, SSA 1-97) and FEMA Guidelines. This is a local study and has not been submitted to FEMA. 1.2 Project Authority The State of Arizona has delegated the responsibility to each county flood control district to adopt floodplain regulations designed to promote the public health, safety and general welfare of its citizenry as provided under the Arizona Revised Statutes, Title 48, Chapter 21, Article 1, Sections 48-3601 through 3627. More specifically, A.R.S. 3609 directs county flood control districts to adopt floodplain regulations that: A. Regulate all development of land, construction of residential, commercial or industrial structures or uses of any kind which may divert, retard or obstruct flood water and threaten public health or safety or the general welfare; and B. Establish minimum flood protection elevations and flood damage prevention requirements for uses, structures and facilities which are vulnerable to flood damage; and C. Comply with state and local land use plans and ordinances, if any. In conformance with A.R.S. 3609, this ordinance provides for protection of the public health safety and welfare by regulation of flood and erosion hazard areas to control flood hazards and prevent repetitive loss from flood damage. D. The flood hazard areas of Pima County are subject to periodic inundation which may result in loss of life and property, create health and safety hazards, disrupt commerce and governmental services, require extraordinary public expenditures for flood protection and relief, and impair the tax base, all of which adversely affect the public health, safety, and general welfare. E. These flood losses are caused by the cumulative effect of obstructions in areas of special flood hazards which increase flood heights, flow velocities, and cause flood and erosion damage. Uses that are inadequately flood-proofed, elevated, or otherwise protected from flood damage, also contribute to the flood loss. (Ord. 2005 FC-2 § 2 (part), 2005). 3 Section 16 of the Pima County Ordinance describes the provisions for floodplain regulation in Pima County. This study has been prepared by the Pima County Regional Flood Control District (RFCD): Pima County Regional Flood Control District 97 East Congress, Tucson, AZ 85701 The project was prepared by: Dave Stewart, EIT, Civil Engineering Assistant Pima County Regional Flood Control District 97 East Congress, Tucson, AZ 85701 1.3 Project Location The Casas Adobes (CSA) study area is located within Federal Emergency Management Agency (FEMA) Flood Insurance Rate Map (FIRM) panels 04019C1680L, 1660L, and 1667L. The FEMA-designated “Zone A” flood-hazard area is specified for the length of the Casas Adobes wash from upstream of the W. Sunset Rd. bridge to downstream of W. Orange Grove Rd (Figure 1.2). A Letter of Map Revision with effective date of April 10, 2001 displayed updated topographic information along the CSA from approximately 420 feet north of Sunset Rd. to approximately 1200 ft South of Orange Grove Rd. The objective of this TDN is to provide discharges and floodplain limits along the CSA using updated topographic data, hydrologic modeling, and hydraulic modeling. The detailed study reach for the Casas Adobes Wash (CSA) is from the W. River Rd. Bridge at the downstream boundary to N. Oracle Rd at the upstream end. The CSA enters the study reach from the northeast and a tributary to the CSA converges in Section 10 of Township 13 South, Range 13 East, Pima County, Arizona (Figure 1.2). A levee has been constructed on the west bank of the CSA south of the confluence, and the channel is lined immediately upstream of the Sunset Rd. Bridge to the CSA outlet at the Rillito River (Section 15, Township, 13 South, Range 13 East). 1.4 Hydrologic and Hydraulic Methods A hydrologic analysis was performed to determine the 100-year return period discharge at concentration points along the CSA using the Hydrologic Engineering Center’s Hydrologic Modeling System (HEC-HMS) and PC-HYDRO for the tributary. The hydraulic analysis was performed to delineate floodplain limits along the study reach of the CSA using the Hydrologic Engineering Center’s River Analysis System (HEC-RAS) 4 (USACE 2002) and FLO2D models in the upstream distributary flow areas. A box culvert is located at the CSA crossing with W. Orange Grove Rd, and bridges are located at W. Sunset Rd and W. River Rd. Storm drains are located at the W. Ina Rd. crossing that have an outlet downstream of the N. Oracle Rd. crossing, where the hydraulic study begins. The attenuation of the peak discharge from culverts and bridges was not included in the calculation of the discharge to provide a conservative estimate. 1.5 Acknowledgments This study relied on assistance of RFCD staff, who were integral to the development of the models and maps. 1.6 Study Results The CSA was divided into 25 sub-basins, and discharges were calculated at significant confluences for floodplain mapping (Fig. 1.2). The estimated discharges are 1474.0 cfs for the main reach at Las Lomitas Rd. (CP A) with an area of 1.42 mi2, a discharge of 1133.0 cfs for the tributary at La Lomitas Rd. (CP B) with an area of 0.518 mi2, a discharge of 1987.2 cfs for the confluence with the Rillito (CP C) with an area of 2.22 mi2, a discharge of 1363.3 cfs for the main reach at La Canada Rd. (CP D) with a drainage area of 1.06 mi2, and a discharge of 479.0 cfs for the tributary at La Canada Rd. (CP E) with a drainage area of 0.15 mi2. 5 Figure 1.1 Watershed Map Casas Adobe Wash MAGEE ! ( Discharge Point Contour 10 ft. Subbasin CSAA001 CSAA002 CSAA003 CSAA004 CSAA005 CSAA006 CSAA007 CSAA008 INA CSAA009 CSAA010 SK CSAA011 YL E IN CSAA012 CSAB001 CSAB002 CSAB003 CSAB004 CSAB005 CP E CSAB006 ! ( CSAB007 CSAB008 CSAB009 CSAC001 CSAC002 ! ( CP D CSAC003 CSAC004 ORANGE GROVE Aerial : 2010 Pictometry Topo: 2008 Pima Association of Governments Datum: NAVD 1988 ORACLE ! (! ( Index Map Scale 1:5,250,000 1ST CP B CP A LA CANADA LA CHOLLA Pima County Index Map The information depicted on this display is the result of digital analyses performed on a variety of databases provided and maintained by several governmental agencies. The accuracy of the information presented is limited to the collective accuracy of these databases on the date of the analysis. The Pima County Regional Flood Control Department makes no claims regarding the accuracy of the information depicted herein. This product is subject to the Department of Transportation Technical Services Division's Use Restriction Agreement. Pima County Regional Flood Control District ER ! ( RIV CP C 1,000 500 0 01/2011 \\gislib\rfcd\projects\imd\xavi\mxd\AKITSU\Casas_Adobe_wash\Casas_Adobe_Wash_Fig1_1.mxd 1,000 Feet Figure 1.2 Study Limit Casas Adobe Wash MAGEE ORACL E CSAA011 ORACL E MAGEE CSAA009 ( ! Discharge Points River CSAA010 Subbasin Boundary Existing FEMA Floodplain INA CSAA008 ZONE A INA ZONE AE CSAA012 E IN YL SK CSAB008 E IN YL SK CSAA007 CSAB009 LA CANADA ZONE X - SHADED Aerial : 2010 Pictometry CSAB006 CSAA005 CSAA006 CSAB007 CSAB004 CSAB005 CSAB003 ORANGE GROVE CSAA003 ( ! CP D CSAA004 Pima County Index Map CSAB002 CSAA002 CSAA001 1ST CSAB001 LA CHOLLA Index Map Scale 1:5,250,000 !! ( ( CSAC004 CP B CP A The information depicted on this display is the result of digital analyses performed on a variety of databases provided and maintained by several governmental agencies. The accuracy of the information presented is limited to the collective accuracy of these databases on the date of the analysis. The Pima County Regional Flood Control Department makes no claims regarding the accuracy of the information depicted herein. CSAC002 This product is subject to the Department of Transportation Technical Services Division's Use Restriction Agreement. Pima County Regional Flood Control District CSAC003 RIVE R 1,0 00 500 0 RIVER Study Limit ( ! CP C ORACLE CSAC001 01/2011 \\gislib\rfcd\projects\imd\xavi\mxd\AKITSU\Casas_Adobe\Casas_Adobe_wash_Fig1_2.mxd 1,0 00 Fe et Figure 1.3 Soil Classification Casas Adobe Wash MAGEE ORACL E CSAA011 Subbasin ORACL E Soil Classification CSAA009 Soil Group: A (100%), ARIZO-RIVERWASH COMPLEX, 0 TO 3 PERCENT SLOPES Soil Group: A (100%), RIVERWASH CSAA010 Soil Group: A (100%), VINTON SANDY LOAM Soil Group: A (53%) B (47%), VINTON-ANTHONY SANDY LOAMS Soil Group: B (100%), CSAA008 INA Soil Group: B (100%), ANTHONY FINE SANDY LOAM, 0 TO 3 PERCENT SLOPES Soil Group: B (100%), ANTHONY GRAVELLY SANDY LOAM,1 TO 3 PERCENT SLOPES Soil Group: B (100%), GILA LOAM, 0 TO 1 PERCENT SLOPES INA CSAA012 E IN YL SK CSAB008 Soil Group: B (100%), GILA SANDY LOAM CSAA007 Soil Group: B (100%), GRABE LOAM CSAB009 E IN YL SK CSAB006 CSAA005 CSAA006 CSAB004 CSAB005 CSAB003 LA CANADA CSAB007 Soil Group: B (100%), PINALENO-STAGECOACH COMPLEX, 5 TO 16 PERCENT SLOPES Soil Group: B (50%) C (50%), PALOS VERDESSAHUARITA COMPLEX, 2 TO 8 PERCENT SLOPES Soil Group: B (82%) C (18%), PINALENO-STAGECOACHPALOS VERDES COMPLEX, 10 TO 35 PERCENT SLOPES Soil Group: C (100%), ROUGH BROKEN LANDPALOS VERDES COMPLEX, 0 TO 60 PERCENT SLOPES Soil Group: C (50%), D (50%) Soil Group: C (53%) D (47%), PALOS VERDESJAYNES COMPLEX, 2 TO 8 PERCENT SLOPES ORANGE GROVE Aerial : 2008 Pima Association of Governments CSAA003 CSAA004 Pima County Index Map CSAB002 CSAA002 CSAA001 1ST CSAB001 LA CHOLLA CSAC004 CSAC002 Index Map Scale 1:5,250,000 The information depicted on this display is the result of digital analyses performed on a variety of databases provided and maintained by several governmental agencies. The accuracy of the information presented is limited to the collective accuracy of these databases on the date of the analysis. The Pima County Regional Flood Control Department makes no claims regarding the accuracy of the information depicted herein. This product is subject to the Department of Transportation Technical Services Division's Use Restriction Agreement. Pima County Regional Flood Control District 990 495 0 CSAC003 RIVER CSAC001 E RIV 11/2010 R \\gislib\rfcd\projects\imd\xavi\mxd\AKITSU\Casas_Adobe\Casas_Adobe_wash_Fig1_3.mxd 990 Feet Section 2 FEMA Forms 2.1 Study Documentation Abstract for FEMA submittals 2.1.1 Date Study Accepted: This study has not been submitted to FEMA.__ 2.1.2 Study Contractor: Planning and Development Division, Pima County Regional Flood Control District 97 East Congress, Tucson, AZ 85701 (520) 243-1800 Prepared by Dave Stewart, EIT, Civil Engineering Assistant. 2.1.3 Local Technical Reviewer: Planning and Development Division, Pima County Regional Flood Control District 97 East Congress, Tucson, AZ 85701 (520) 243-1800 2.1.4 Reach Description A segment of the CSA study reach is located within a FEMA-designated “Zone A” floodhazard area, as depicted on FIRM Map Panel Numbers 04019C1660L and 1667L (February 8, 1999). The detailed study reach of the CSA begins immediately downstream of N. Oracle Rd. and ends at the W. River Rd. bridge. The study reach of the CSA is primarily a sand channel with desert brush in the channel and in the overbanks areas. 2.1.5 USGS Quad Sheets Not available for this study 2.1.6 Unique Conditions and Problems None. 9 2.1.7 Coordination of Peak Discharges The 100-year regulatory discharge rates at the concentration points along the study reach were computed using HEC-HMS and PC-Hydro for CP B and E. The HEC-HMS discharges assumed no base flow in the watersheds and no transmission losses within the reaches. All reaches were modeled with HEC-RAS. The discharge rates were acceptable per Evan Canfield, Pima County Regional Flood Control District Project manager. 2.2 FEMA Forms This is a local study and no FEMA forms are included in this TDN. Section 3 Survey and Mapping Information 3.1 Field Survey Information A box culvert is located at the Casas Adobes Wash crossing at W. Orange Grove Rd, and bridges are located at W. Sunset Rd and W. River Rd. Storm drains are located at the W. Ina Rd. crossing that have an outlet at the N Oracle Rd. crossing. A dip crossing is located at N. La Canada Rd. 3.2 Mapping The topographic data was obtained using GeoRas and ArcGIS. A triangular Irregular Network (TIN) derived from 2008 Light Detection and Ranging (LiDAR) data was used for the analysis. The following data was used in this TDN; Projection = State Plane, Arizona Central Zone Datum = NAD83 HARN Units = International Feet North American Vertical Datum of 1988 (NAVD, 1988) The contour interval of the topographic map is 2 feet. Section 4 Hydrology 4.1 Method Description The 100-year peak discharges at CSA concentration points with drainage area greater than 1 mi2 (CP A, C, D) were calculated using the Hydrologic Engineering Center’s 10 Hydrologic Modeling System, (HEC-HMS) version 3.1.0, and the peak discharges at concentration points with drainages areas less than 1 mi2 (CP B and E) were found using PC-Hydro. The HEC-HMS model parameters for rainfall, topography, soil, vegetation, and channel characteristics were determined according to the Pima County Regional Flood Control District Technical Policy 018 (Tech-018). Tech-018 is included in Appendix A. The HEC-HMS and PC-Hydro models are included in Appendix D. 4.2 Parameter Estimation 4.2.1 Drainage Area As mentioned in 3.2, topographic data was derived from a TIN created from 2008 LiDAR data. ArcGIS was used to delineate the sub-basins. The watershed map is shown in Figure 1.1. 4.2.2 Watershed Work Map ArcGIS was used to determine drainage areas from 2008 LiDAR data in Figure 1.1. Subbasins were delineated for the hydrologic analysis at CP A, C, and D in HEC-HMS, and for the hydrologic analysis at CP B and CP E in PC-Hydro. 4.2.3 Gage Data No gage data were used in this TDN. 4.2.4 Statistical Parameters No statistical parameters were used in this TDN. 4.2.5 Precipitation According to Tech-018, the design storm should be used that produces the higher discharge between the 100-yr 3-hour SCS Type II distribution and the 100-yr 24-hr SCS Type I distribution. The 100-yr 3-hour SCS Type II distribution was found to produce the higher discharge on the CSA. The NOAA Atlas 14, upper 90% confidence interval precipitation frequency estimate values (NOAA 14 rainfall) were used to determine point 3-hour rainfall depth for the 11 CSA watershed. The point rainfall depth for the 3-hour storm was obtained, based on the coordinates of the centroid of the watershed. Area reduction factor was applied to watersheds larger than 1 square mile as noted in Tech-018. The 3-hour rainfall depth for the CSA watershed is 3.17 inches. The area reduction factors are 0.946, 0.938, and 0.970 for CP A, C and D respectively. 4.2.6 Physical Parameters The physical parameters for the sub-basins and reaches of the HEC-HMS model are summarized in Tables 1 and 2. As mentioned in 4.1, all the methods and parameters were determined based on Tech-018. Table 1 summarizes the method used for a HEC-HMS analysis. Table 4.1 Methods used for a HEC-HMS analysis Rainfall Depth Rainfall Distribution Rainfall Loss Time of Concentration Transform Routing Selected Method NOAA 14, upper 90% Confidence Interval 3-hr SCS Type II Storm SCS Curve number SCS Segmental Method SCS Unit Hydrograph Modified-Puls The SCS Curve Number (CN) method was utilized as a rainfall loss method in the HECHMS model. The CN was determined using the Curve Number tables and Hydrologic Soils Group maps associated with the PC Hydro User Guide (Arroyo Engineering, 2007). The CN was not adjusted for rainfall intensity or antecedent moisture conditions. The SCS Unit Hydrograph method was used as a transform method. Impervious cover was determined using the 2008 PAG aerial photographs. The combination of the kinematic wave time of concentration method and the U.S. Natural Resources Conservation Service (NRCS) segmented Time of Concentration (Tc) calculation (USDA-NRCS, 1986) was used to determine Tc, based on the recommendation on Tech-018. The Tc was calculated by summing the travel time for sheet flow, shallow concentrated flow and channel flow. The Tc for sheet flow was estimated using the kinematic wave equation. Manning’s roughness coefficient for sheet flow was obtained using Table 3-1 in Technical Release 55, Urban Hydrology for Small Watersheds (USDA-NRCS, 1986). The detail of the Tc calculation is included in Appendix D. 12 Table 4.2. Physical Parameters for Sub-Basins 2 Sub-basin Area (mi ) A1 0.068 A2 0.059 A3 0.085 A4 0.145 A5 0.065 A6 0.126 A7 0.101 A8 0.076 A9 0.249 A10 0.276 A11 0.126 A12 0.040 B1 0.035 B2 0.074 B3 0.056 B4 0.049 B5 0.039 B6 0.052 B7 0.111 B8 0.064 B9 0.039 C1 0.055 C2 0.080 C3 0.020 C4 0.130 CN 86.1 89.0 87.4 89.3 89.3 87.3 86.1 86.5 85.2 86.5 83.1 88.7 87.3 88.8 89.4 89.3 89.4 89.4 89.4 88.6 87.5 83.0 86.7 83.5 88.6 Initial Abstraction (in) 0.249 0.182 0.211 0.178 0.170 0.217 0.225 0.172 0.256 0.258 0.383 0.146 0.186 0.177 0.163 0.162 0.198 0.187 0.171 0.175 0.204 0.293 0.276 0.373 0.200 Imp% 22.1% 26.9% 26.3% 26.4% 30.0% 24.8% 29.5% 44.5% 24.9% 16.9% 5.0% 43.4% 35.5% 30.1% 32.0% 33.3% 16.7% 21.3% 28.5% 32.3% 28.3% 26.4% 9.4% 5.0% 22.5% Lag time (min) 10.12 15.50 10.04 18.17 13.53 12.92 15.72 10.33 13.35 14.70 11.59 11.84 6.78 10.81 16.49 9.34 9.38 12.53 19.88 16.81 17.45 15.45 11.94 5.46 24.68 Runoff from sub-basins was routed using the Modified-Puls method. A storage discharge table for the channel routing was developed using the cross sections and slopes in HECRAS. The number of subreaches was calculated using the following method: L ...................eq.1 T Vw  1.5 * Vave .........eq.2 Vave  K L ...................eq.3 Vw Therefore, T K ...................eq.4 1.5 K N  ..................eq.5 t where Vave is average flow velocity, L is reach length, T is average travel time, Vw is the wave celerity (a conversion factor of 1.5 is used for natural channels), K is hydrograph travel time, Δt is the time interval for computations in the model, and N is the number of steps in the routing. Eq.4 was obtained from Eq.1, 2, and 3. 13 Table 4.3. Physical Parameters for Reaches Sub-basin Number of subreaches RCSA001 12 RCSA002 7 RCSA003 5 RCSA004 8 RCSA005 5 RCSA006 6 RCSA007 4 RCSA008 3 RCSA009 8 RCSA010 14 RCSA011 7 RCSA012 4 RCSA013 5 RCSA014 4 4.3 Problems Encountered During the Study 4.3.1 Special Problems and Solutions There were no problems with the hydrologic modeling. 4.3.2 Modeling Warning and Error Messages The time interval of the rainfall data used in this study is 5 minutes, while the simulation time interval is 1 minute. The HEC-HMS model interpolated the 5-minute time interval of the rainfall data to 1-minute time interval. Warnings were produced in the HEC-HMS model stating that each hyetograph gage with 5 minute interval was interpolated to a simulation time interval of 1 minute.; 4.4 Calibration No calibration was conducted in this study. 4.5 Final Results 4.5.1 Hydrologic Analysis Results 14 The 100-year peak discharges at the concentration points along the CSA were determined using the HEC-HMS model. The results are summarized in Tables 4 and 5. Table 4.4 Summary of sub-basin discharges. Sub-basin Area (mi2) Rainfall Depth (in) Runoff Depth (in) A1 A2 A3 A4 A5 A6 A7 A8 A9 A10 A11 A12 B1 B2 B3 B4 B5 B6 B7 B8 B9 C1 C2 C3 C4 0.068 0.059 0.085 0.145 0.065 0.126 0.101 0.076 0.249 0.276 0.127 0.040 0.035 0.074 0.057 0.049 0.039 0.052 0.111 0.064 0.039 0.055 0.080 0.020 0.130 3.17 3.17 3.17 3.17 3.17 3.17 3.17 3.17 3.17 3.17 3.17 3.17 3.17 3.17 3.17 3.17 3.17 3.17 3.17 3.17 3.17 3.17 3.17 3.17 3.17 2.05 2.29 2.18 2.31 2.34 2.16 2.13 2.33 2.02 2.02 1.65 2.44 2.27 2.31 2.37 2.37 2.23 2.09 2.34 2.32 2.21 1.64 1.92 1.68 2.22 Peak Discharge (cfs) 175.9 136.0 231.7 307.8 163.8 304.0 217.1 218.5 556.1 584.6 248.9 110.9 113.3 205.2 129.9 147.7 111.6 123.8 225.1 142.2 80.4 91.9 178.9 51.3 216.8 Table 4.5. Summary of 100-yr Peak Discharge Values Concentration Point Area (mi2) Name Location CP A Main Reach at Las Lomitas 1.42 CP B* Tributary at Las Lomitas 0.52 CP C At the Rillito 2.22 CP D Main Reach at N. La Canada Rd. 1.06 CP E* Tributary at La Canada Rd. 0.15 *Runoff volumes are not directly calculated in PC-Hydro. 100-yr Peak Discharge (cfs) 1474.0 1133.0 1987.2 1363.3 479.0 Runoff Volume (in) 1.99 Time of Peak (min) 134 1.95 1.98 142 122 4.5.2 Verification results The 100-yr peak discharge was compared with discharges estimated from the USGS Regression Equation 13 (RRE13) (Thomas et al., 1997) (Table 4.8). The comparison shows that the modeled 100-yr peak discharge is slightly lower than the RRE13 discharge for CP A and CP C, possibly due to the attenuation effects along the main reach. The modeled 100-yr discharge is higher than the RRE13 discharge at CP B, CP D, CP E which may be attributed to the steep slopes and shorter lengths of those reaches and the use of the more conservative PC-Hydro estimate for CP B and CP E. 15 Table 4.8. Comparison of peak discharge with regional regression equations. Name CP A CP B CP C CP D CP E Concentration Point Location Main Reach at Las Lomitas Tributary at Las Lomitas At the Rillito Main Reach at N. La Canada Rd. Tributary at La Canada Rd. Area (mi2) 1.42 0.52 2.22 1.06 0.15 100-yr Peak Discharge USGS RRE13 Qp (cfs) (cfs) 1474.0 1581.0 1133.0 796.6 1987.2 2092.5 1363.3 1307.9 479.0 297.3 Section 5 Hydraulics 5.1 Method Description The hydraulic modeling for the CSA wash was performed using FLO-2D, Hec-Ras, Version 4.0 (HEC-RAS), and HEC-GeoRAS Version 4.1.1. 2008 LiDAR data was used to create a Triangular Irregular Network (TIN) for the detailed study area of the CSA wash. The locations of the stream centerline, crosssections, and banks of the CSA wash were determined using ArcGIS and 2008 PAG aerial photos. The physical attributes of the wash were digitized in ArcGIS using the HEC-GeoRAS extension and then exported to HEC-RAS to create geospatially referenced geometric data (cross sections, and reach lengths). Other parameters for the steady-state analysis, such as Manning’s n-values, culvert data, expansion and contraction coefficients, boundary condition, and ineffective flow areas were manually input into HEC-RAS. The hydraulic data obtained from HEC-RAS were then imported into HEC-GeoRAS to delineate a floodplain in the study area. The hydraulic analysis was performed for the study area that includes an area currently mapped as FEMA Zone A. Steady flow analysis was performed to determine 100-year water surface elevations in the study area by using HEC-RAS. As described above, geometric data for HEC-RAS including the stream centerline, cross-sections, river banks, and culverts were obtained using HEC-GeoRAS. The HEC-RAS data and shape files (contour lines, flowpath, cross section lines, concentration points, sub-basins, and floodplain limit) from the analysis are included on the CD. The downstream boundary condition was assumed to be critical depth for the HEC-RAS model. Using a normal depth downstream boundary condition was found to have no effect on results above the Sunset Rd. bridge, and therefore the critical depth boundary condition is justified. The reaches upstream of CP A and CP B were found to flow over bank and leave the channel, and therefore FLO-2D was used for those areas. The reaches of the Casas Adobes wash were split into three areas for FLO-2D models which are displayed in Figure 5.1. The HEC-HMS hydrographs from the downstream concentration point were 16 used as the inflow at the upstream boundary of each FLO-2D model. The hydrographs from CP A and B were entered at the top of FLO-2D Area 2, while CP D and E were used at the top of FLO-2D Area 1, and the hydrograph for CP D was used at the top of FLO-2D Area 3 (which results in a breakout flow path that connects to the tributary in Area 1). A base floodplain Manning’s n value of 0.045 was used in the FLO-2D models and then calibrated based on the roughness adjustments made by the FLO-2D software. Houses were removed from the effective flow area by using the area reduction factors in FLO-2D. The FLO-2D models are included in Appendix E. Figure 5.1. The study areas for the three FLO-2D models. 5.2 Work Study Maps The work study maps are included as Exhibits. 17 5.3 Parameter Estimation 5.3.1 Roughness Coefficients The Manning’s n values were assigned based on USGS publications on roughness coefficients for Southern Arizona (Phillips and Tadayon, 2006). A Manning’s n value of 0.045 was assigned for the channel and 0.055 was assigned for the overbank due to scattered desert brush. In FLO-2D, the n values were calibrated based on the roughness adjustment performed by the FLO-2D software. 5.3.2 Expansion and Contraction Coefficients The channel of the Casas Adobes Wash is assumed to have gradual transitions and default expansion and contraction coefficients of 0.3 and 0.1 were used respectively. 5.4 Cross-Section Description HEC-RAS Cross sections were created using GeoRAS at changes in channel geometry from the 2008 LiDAR data. The cross-section lines were drawn to be perpendicular to flow paths in Geo-RAS and ArcGIS. Cross sections were not created for FLO-2D. 5.5 Modeling Consideration 5.5.1 Hydraulic Jump and Drop Analysis No hydraulic jump or drop was shown in the analysis of this study. 5.5.2. Bridges and Culverts The Sunset Rd. bridge was modeled at the downstream end of the study area using the “As-built” plans for the Casas Adobes wash levee at Riverside Crossing (Environmental Engineering Consultants, Inc. 12/18/98) included in Appendix C. The bridge at Sunset Rd. consists of four 12’ x 8’ cells. 5.5.3 Levees and Dikes The Riverside Crossings Levee is located on the west bank of the CSA wash from immediately upstream of W. Sunset Rd. up to Las Lomitas Rd and was accredited by FEMA on July 24, 2009 (Appendix B). The 2008 LiDAR data were used for the levee 18 features in HEC-RAS cross sections. “As-built” plans for the CSA levee (12/18/98) are included in Appendix C. 5.5.4 Island and Flow Splits FLO-2D was used for the reaches of the Casas Adobes wash where significant flow splits and breakouts were found. 5.5.5 Ineffective Flow Areas Ineffective flow areas were defined in HECRAS for areas of cross sections that were not hydraulically connected until the water surface elevation exceeded a topographic feature. Ineffective flow areas were set as permanent for large areas not connected to the channel that would otherwise cause instability in the model when the water surface elevation exceeded the ineffective flow elevation. 5.6 Floodway Modeling No floodway modeling was performed in this study. 5.7 Problems Encountered 5.7.1 Special Problems and Solutions There are no special problems in the study limit. 5.7.2 Model Warnings and Errors The FEMA guidelines state that it is required to run hydraulic models for the subcritical flow condition. Since areas of the CSA wash have steep slopes and a lined channel, the flow regime of the CSA is expected to exhibit critical flow at some locations. The HECRAS modeling produced some warnings stating “During the standard step iterations, when the assumed water surface was set equal to critical depth, the calculated water surface came back below critical depth. This indicates that there is not a valid subcritical answer.” The program defaulted to critical depth at several HEC-RAS cross-sections along the lower reach of the CSA. Most of the warnings force a critical solution which is reasonable for these steep watercourses. A summary of errors is available in Appendix E. 19 The warnings stating that “The energy equation could not be balanced within the specified number of iterations. The program used critical depth for the water surface and continued on with the calculations”, “The energy loss was greater than 1.0 ft (0.3 m) between the current and previous cross section. This may indicate the need for additional cross sections”, and “The conveyance ratio (upstream conveyance divided by downstream conveyance) is less than 0.7 or greater than 1.4. This may indicate the need for additional cross sections” are produced at some locations in the Casas Adobes HECRAS study reach. These warning messages were expected due to the steep slopes of the CSA wash. All the warning messages in the HEC-RAS modeling are included in Appendix E. 5.8 Calibration The FLO-2D models for the Casas Adobes wash were calibrated for roughness to improve model stability and speed. The TIME.OUT and ROUGH.OUT files were reviewed and the cells causing increases in time steps were replaced with the higher roughness values. 5.9 Final Results 5.9.1 Hydraulic Analysis Results The Casas Adobes wash 100-yr floodplain is shown in Exhibit 1, Sheets 1 through 3. The HEC-RAS model of the CSA is included in Appendix E. The lower reach of the CSA (from CP A and B down to CP C) is considered a confined wash at some locations and additional floodplain restrictions may apply. The ratio of the average width of the 100-yr floodplain to the 25-yr floodplain was found to be 1.22 for the lowest reach (lower than the 1.25 criterion), and at some locations the overbanks are higher than 1.5 times the 100-yr flow depth. The CSA is not considered a confined wash in the reaches above CP A and B. 5.9.2 Verification of Results The floodplain limit obtained by this study was compared to the current FEMA floodplain limit. The proposed floodplain approximately follows the existing floodplain limit; however, this study extends further north and covers both the tributary as well as the main reach. The results within in the current FEMA floodplain suggest that the proposed floodplain limit is reasonable based on the new topographic data of the Casas Adobes Wash. 20 Section 6 Erosion and Sediment Transport No erosion and sediment transport study was conducted in this study. Section 7 Draft FIS Report Data 7.1 Summary of Discharges Table 7. Summary of Discharges Name CP A CP B CP C CP D CP E Concentration Point Location Main Reach at Las Lomitas Tributary at Las Lomitas At the Rillito Main Reach at N. La Canada Rd. Tributary at La Canada Rd. Area (mi2) 1.42 0.52 2.22 1.06 0.15 100-yr Peak Discharge (cfs) 1474.0 1133.0 1987.2 1363.3 479.0 7.2 Floodway Data Not applicable. 7.3 Annotated Flood Insurance Rate Map Not applicable. 7.4 Flood Profiles Flood profiles are included in Appendix E. 21 2350 23 70 SEE SHEET 2 OF 3 236 40 Exhibit 1 100-year Floodplain with cross sections Casas Adobes Wash Sheet 1 of 3 0 239 5 2360 23 2370 0 23 8 G 2360 M N 50 O 23 AN PO 55 5 2350 23 236 2340 EL O 2340 A N O R 235 0 U TI B E ESCONDIDO LL A C R O 23 7 0 N MONTEBELLA U 35 ! ( 0 23 3 FOUNTAINS 232 2320 CasasAdobes BFE Contours 1ft 5 2310 C 232 L AL E CasasAdobes BFE Contours 5ft O KIN Cross Sections 0 23 0 23 2 2300 2305 L CA 10 L I BU T E R ON Study Area ! ( 381 6 Shallow Flooding Zone 0 CP A Casas Adobes FLO2D Floodplain BFE FlowDepth 2300 3620 2296 .291 229 6 LAS LOMITAS =>0.200 .874 LA CANADA 2295 .235 3478 2292 .566 3413 229 1 U V V U V U V U V U V U V U V U V U V U VU U V 3329 2290.082 2289.499 3265 Aerial : 2010 Landiscor Aerial Imagery 2287.365 3100 E ORACLE JAYN 2978 0 227 2861 2824 2765 2717 2608 2506 2270.547 2284.204 2282.936 E V 2280.318 2276.982 Topo: 2008 Pima Association of Governments Datum: NAVD 1988 2275.994 2271.853 227 0 2270.132 2393 L A A IST 2285.203 S STATION 2661 U V SUNSET V U A SH 2286.184 3037 2270 =>2.000 2287.996 3175 0 =>1.000 2310 0 48 2330 0 23 .806 231 0 2270 2290.9 =>0.500 GRANDE 0 0 V U 2 23 0 3725 2300 0 23 0 23 22 9 U V V U V U V U V U ! ( CP B 2305 0 230 2300 Casas Adobe 100-yr Floodplain 3534 7 22 River LAS LOMITAS 15 23 2280 Contour10ft 2325 2310 2320 0 2310 LA CHOLLA 5 23 235 0 2315 2320 2320 2320 2320 2320 RUDASILL 2330 23 30 2350 0 PLACITA C 0 2 23 Discharge Points 2008 Contour 2ft 2335 232 RUDASILL HICO 23 3 0 B TI 2330 A IT 23 2340 2325 C 0 234 0 2345 A CORONA PANORAMA 0 236 PL 234 2330 2330 45 50 23 23 FOUNTAIN PLAZA 2335 A VI IG T LA O SUNSET 44 6.1 226 E KLAMATH COACHWHIP HOPBUSH LA CANADA PAINTBRUSH Index Map Scale 1:1,500,000 WHISPERING HILLS POMONA ORACLE JAYNES STATION MESQUITE B AF ER RIV The information depicted on this display is the result of digital analyses performed on a variety of databases provided and maintained by several governmental agencies. The accuracy of the information presented is limited to the collective accuracy of these databases on the date of the analysis. The Pima County Department of Transportation Technical Services Division makes no claims regarding the accuracy of the information depicted herein. HUDSON HUDSON This product is subject to the Department of Transportation Technical Services Division's Disclaimer and Use Restrictions. Pima County Regional Flood Control District 0 100 200 NEOSHO RIV ER ROLLER COASTER ER RIV T GEN RO LE B OK SUNRIVER HANSEN ! ( E FLINT ALDER GROVE L R E T WA CP C Pima County Index Map KEVY 2260.992 O S Q UE LA CHOLLA 1310 OK POMONA V U AN 2264.24 EB EC 1510 K EN N 9 170 WILLOW THICKET LITTLE RIVER UU V V BRAMBLE BROOK V U 18 64 RO ESCONDIDO AM WHITETHORN RE D ST RL AN R BE 2 .33 67 2 2 LV E M SI TRINITY 2110 CU V U CHEYENNE 2268.356 Pima County Regional Flood Control 97 East Congress Street - 3rd Floor Tucson. Arizona 85701-1207 (520)243-1800 - FAX (520)243-1821 http://www.rfcd.pima.gov 10/2011 gislib\rfcd\projects\imd\xavi\mdx\AKITSU\Casa_Adobe\Casas_Adobes _Exhibit_1_s1of3.mxd 400 Feet Exhibit 1 100-year Floodplain with cross sections Casas Adobes Wash Sheet 2 of 3 MAXIMILIAN BA R AR GIACONDA PENNY M O AI KH PALOMA KH AI BA CASPIAN CASPIAN R ! ( CHULA VISTA KENANNA 2465 247 PALER MIDDLETON 5 2455 2450 24 70 2465 River 70 2440 24 Study Area 70 2450 2430 S LO OS L I F 2465 ME 2445 2410 2465 Shallow Flooding Zone 24 2460 RA N SESA CP E Casas Adobe 100-yr Floodplain 2430 HAR ! ( 2460 0 2455 243 2435 MONTENEGRO 65 LA CO NI LA CANADA N SA 2435 0 24 0 SAN IGNACIO 2420 2415 LA CANADA 2400 LEONARDO DA VINCI 2420 2400 0 23 8 CAMINO DE COROZAL 2360 2390 23 SAHARA PALMS 80 VIA CABALLO This product is subject to the Department of Transportation Technical Services Division's Disclaimer and Use Restrictions. Pima County Regional Flood Control District IA 75 SAFARI The information depicted on this display is the result of digital analyses performed on a variety of databases provided and maintained by several governmental agencies. The accuracy of the information presented is limited to the collective accuracy of these databases on the date of the analysis. The Pima County Department of Transportation Technical Services Division makes no claims regarding the accuracy of the information depicted herein. 0 100 200 E 70 LL 23 65 CA 23 DE LM ED 2370 0 23 7 EL O CALLE TIBURON 55 2360 G Index Map Scale 1:1,500,000 0 AN VIA TIERRA VIA RANCHERO MONTEBELLA IS 5 MONTEBELLA 23 0 CALLE KINO 23 50 235 0 OA S A 236 50 2330 2440 2440 2395 23 9 2380 A MONTEBELL 2380 2370 2360 0 90 9 23 23 5 M AL AG A 238 2360 2350 VIA HACIEND 5 90 2360 Pima County Index Map 0 23 2360 23 23 45 0 24 5 2370 0 CORONA 23 0 237 235 0 CA 2370 7 23 2350 2450 S 24 1 ANTAS 2400 PLACIT A DE S 0 239 0 ST A VI A LL O H C 00 RAN PLACITA PLACITA DE ZACATAL 23 2340 SEE SHEET 3 OF 3 5 238 60 2360 23 2335 239 2385 2350 2345 2340 60 0 24 240 95 BA R ALINADA 2375 40 50 0 23 CITA RRE O N MINO DE TO HOSPITAL 23 24 2425 0 24 24 65 PLACITA PLA 0 2350 235 0 0 CP D CARAVAN 2370 2355 5 23 ! ( APPIAN SAN MIGUEL 2390 PLACITA DE OCAMPO 236 0 5 23 0 ORANGE GROVE CA 60 3 2 25 2370 2380 23 2360 Datum: NAVD 1988 SANTO DOMINGO 2410 2400 2360 Topo: 2008 Pima Association of Governments 30 24 75 ORANGE GROVE MEDICAL 45 2425 5 90 0 Aerial : 2010 Landiscor Aerial Imagery SAN LUCAS 85 7 23 244 45 2400 23 24 0 23 C AL TO S SANTO DOMINGO 23 VISTA LEJOS NA LU S 10 240 2410 238 C O R O 0 2435 LO S AS 24 2420 2380 23 8 AN 2440 2430 24 0 240 2410 =>1.000 =>2.000 24 LA 40 EL 35 EB 24 NT 2455 0 242 =>0.500 2460 2450 MO 45 0 24 L LOS ALTOS 24 1 24 2440 2420 AH Casas Adobes FLO2D Floodplain BFE FlowDepth =>0.200 2425 2440 AM Cross Sections 24 C CasasAdobes BFE Contours 5ft 60 2470 MO 24 2465 POMONA IM CasasAdobes BFE Contours 1ft 5 GI SS ED 245 MA M 2445 CA TARANTULA RANCH 2470 AH Contour10ft DESERT HARBOR 2465 SIM 2008 Contour 2ft 2475 CHULA VISTA CAS Discharge Points SEE SHEET 1 OF 3 PANORAMA Pima County Regional Flood Control 97 East Congress Street - 3rd Floor Tucson. Arizona 85701-1207 (520)243-1800 - FAX (520)243-1821 http://www.rfcd.pima.gov 10/2011 gislib\rfcd\projects\imd\xavi\mdx\AKITSU\Casa_Adobe\Casas_Adobes _Exhibit_1_s2of3.mxd 400 Feet VILLAGE NORTHERN OPUNTA YUCCA VIA VIA PISA SIENA ANTONIETTA INA INA VI FIRENZE VIA PONTE PAMPA INA MONTECATINA VIA ASSISI LA OESTA PASEO DEL NORTE OLD INA Exhibit 1 100-year Floodplain with cross sections Casas Adobes Wash Sheet 3 of 3 ! ( Discharge Points A 2008 Contour 2ft NE VE A ZI Contour10ft GIACONDA CasasAdobes BFE Contours 1ft ALPIA CasasAdobes BFE Contours 5ft 2530 2525 GIACONDA 2500 =>0.200 24 E CAL 2470 TA 24 E 50 CA S CL ORA LOS ARBOLES 2455 LE L OM I 60 EUCALYPTUS Datum: NAVD 1988 CAL 24 AB AZ A S 2460 Topo: 2008 Pima Association of Governments CASAS ADOBES CO RT LE ORAC 75 ANDREA DORIA Aerial : 2010 Landiscor Aerial Imagery 2470 2460 65 =>2.000 FLORENCE 2470 2460 I CO L A 24 =>1.000 UNNAMED NANINI 2470 95 70 70 2465 =>0.500 POMELO 24 24 N TO R U 2490 2485 5 2480 2465 GE G 2505 2485 90 85 247 LOS ALTOS 45 LE ORAC SANTO DOMINGO WHITE ACACIA Pima County Index Map GREER LILLIAN SCHUMAN MARIA 2460 RO V E 2505 MARIA 2500 2480 24 24 2480 2465 SAN N 2450 ORA N 250 5 VISTA PLACITA CHULA VISTA 85 2465 2515 Shallow Flooding Zone Casas Adobes FLO2D Floodplain BFE FlowDepth 2450 24 Casas Adobe 100-yr Floodplain 2510 B 24 SAN LU Study Area 2505 70 2465 0 2515 2510 2495 2490 24 2475 2470 2465 24 252 River CHULA VISTA 2480 MIDDLETON 20 15 2495 25 25 2505 2510 SEE SHEET 2 OF 3 PALOMA Cross Sections VISTA GRANDE ROSE TRE AS UR E Index Map Scale 1:1,500,000 BARCELONA E This product is subject to the Department of Transportation Technical Services Division's Disclaimer and Use Restrictions. Pima County Regional Flood Control District RE E RUSHWOOD UNNAMED YUCCA 0 100 200 BARCELONA ARABIAN ZAMA SPARKL SAFARI POMELO MINARET HA SA OASIS E AGIDIR WINDEMERE MIRAG ME ET M PA L RA SALO NG SAHARA PALMS OR A UNNAMED S CARAVAN The information depicted on this display is the result of digital analyses performed on a variety of databases provided and maintained by several governmental agencies. The accuracy of the information presented is limited to the collective accuracy of these databases on the date of the analysis. The Pima County Department of Transportation Technical Services Division makes no claims regarding the accuracy of the information depicted herein. ORANGE GROVE WILLOWBROOK DESERT PALMS ORANGE GROVE MARAKESH SAN IGNACIO SAN MIGUEL RUSHWOOD MILLBROOK Pima County Regional Flood Control 97 East Congress Street - 3rd Floor Tucson. Arizona 85701-1207 (520)243-1800 - FAX (520)243-1821 http://www.rfcd.pima.gov 10/2011 gislib\rfcd\projects\imd\xavi\mdx\AKITSU\Casa_Adobe\Casas_Adobes _Exhibit_1_s3of3.mxd 400 Feet A.1 Data Collection Summary Aldridge, B. and J. Garrett. 1973. Roughness Coefficients for Stream Channels in Arizona. US Department of the Interior Geological Survey. Tucson, AZ. Arizona Department of Water Resources, Flood Mitigation Section “Requirements for Flood Study Technical Documentation” SS1-97, November 1997 National Weather Service. 1984. Depth-Area Ratios in the Semi-Arid Southwest United States, NOAA Technical Memorandum NWS Hydro-40 Phillips, J., and S. Tadayon. 2006. Selection of Manning’s roughness coefficient for natural and constructed vegetated and non-vegetated channels, and vegetation maintenance plan guidelines for vegetated channels in central Arizona: U.S. Geological Survey Scientific Investigations Report 2006–5108, 41 p. Phillips, J., and T. Ingersoll. 1998. Verification of Roughness Coefficients for Selected Natural and Constructed Stream Channels in Arizona. U.S. Geological Survey Professional Paper 1584. Pima County Regional Flood Control District “Pima County Mapguide Map”, 2008 U.S. Army Corps of Engineers (COE). 2001. HEC-RAS, River Analysis System, Hydraulic Reference Manual, CPD-69, Hydraulic Engineering Center, Davis, CA. U.S. Army Corps of Engineers (COE). 2003. Geospatial Hydrologic Modeling Extension HEC-GeoHMS, (v 1.1) CPD-77, Hydraulic Engineering Center, Davis, CA. U.S. Army Corps of Engineers (COE). 2006. HEC-HMS, Hydrologic Modeling System User’s Manual, (v. 3.1.0) CPD-74A, Hydraulic Engineering Center, Davis, CA. U.S. Department of Agriculture Natural Resources Conservation Service (NRCS), 1986. Urban Hydrology for Small Watersheds, Technical Release 55. Washington, DC. A 2. Referenced Documents Eychaner, J.H., 1984. Estimation of magnitude and frequency of floods in Pima County, Arizona, with comparisons of alternative methods: U.S. Geological Survey WaterResources Investigations Report 84-4142, 69 p. Haan, C.T., Barfield, B.J., Hayes, J.C. 1994. Design Hydrology and Sedimentology for Small Catchments, Academic Press. Thomas, B.E., H.W. Hjalmarson, and S.D. Waltemeyer. 1997. Methods for Estimating Magnitude and Frequency of Floods in the Southwestern United States. USGS Water Supply Paper 2433. 195 p. U.S. Department of Agriculture Natural Resources Conservation Service (NRCS), 1986. Urban Hydrology for Small Watersheds, Technical Release 55. Washington, DC. Appendix B General Documentation and Correspondence Appendix C: Survey Field Notes Appendix D: Hydrology Supporting documentation is included as digital data on the CD. Appendix E: Hydraulics Supporting documentation is included as digital data on the CD. Appendix F: Erosion and Sediment Transport Analysis Supporting Documentation None