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Appendix E Hydrology Report and Water Quality Management Plan
WQMP AND CONCEPTUAL HYDROLOGY REPORT FOR TRACT NO. 20580 FONTANA, CA DECEMBER 15, 2022 Prepared by: United Civil, Inc. 30141 Agoura Road, Suite 215 Agoura Hills, CA 91301-4311 Tel: (818) 707-8648 Fax: (818) 707-864 TABLE OF CONTENTS 1. Introduction ......................................................................................................... 1 1.1. Project Description ............................................................................. 1 1.2. Study Objectives ................................................................................. 1 2. Hydrologic Data .................................................................................................... 1 3. Methodology ........................................................................................................ 2 4. Drainage Analysis ................................................................................................. 2 4.1. Existing Condition ............................................................................... 2 4.2. Proposed Condition ............................................................................ 2 5. Detention ............................................................................................................. 3 6. Water Quality Management Plan (WQMP) .......................................................... 3 7. Conclusion ............................................................................................................ 4 8. References ........................................................................................................... 4 TABLES Table 1 ‐ Existing Hydrology Summary Table 2 ‐ Proposed Hydrology Summary Table 3 ‐ Detention System Summary Table 4 ‐ Detention Outlet Pipe Calculation Table 5 ‐ Detention System Stage‐Volume_Discharge Relation Table 6 ‐ Detention System Routing Table 7 ‐ WQMP Infiltration System Summary Table 8 ‐ WQMP Infiltration System Drawdown Calculation APPENDIX Appendix A ‐ Vicinity Map Appendix B – Master Hydrology Excerpts (TR No. 17389) Appendix C – Hydrologic Data and Design Criteria Appendix D – Rational Method Calculation Appendix E – Unit Hydrograph Calculation Appendix F – Hydrograph Routing Calculation Appendix G – Soil Report Excerpts Appendix H – Design Capture Volume (DCV) Calculation Hydrology Maps 1 1. Introduction 1.1 Project Description The 6.84-acre site is located in the City of Fontana, San Bernardino County, California. The proposed project is located at the Northwest corner of Chase Road. The site is bounded by the developed Tract No. 16724 on the north, Tract No. 18244 on the south, Tract No. 12314 on the west, and Tract No. 17389 on the east (Appendix A). Currently, the site is vacant. Vegetation mainly includes dense weeds. The topo generally slopes in the south and southwest direction. The proposed site consists of 48 single family residential units and a playground. The offsite storm drain improvement plans of Tract No. 17389 included storm drain along the south of the site that was designed to accept the flows from the site [1,2] (Appendix B). Due to the intensified density, proposed peak flow is larger than that specified in master storm drain plan. Thus, an underground detention system is proposed to mitigate the increased flow. To satisfy Water Quality Management Plan (WQMP) requirement of San Bernadino County [3], a separate underground retention system is proposed to infiltrate the Design Capture Volume (DCV) of the site. 1.2 Study Objectives This report was prepared to: 1) Determine 100-year 24-hour peak flow of existing and proposed conditions of the site. 2) Design underground detention system to mitigate increased 100-year peak flow due to intensified density. 3) Design underground infiltration system to satisfy WQMP requirement. The DCV for WQMP was calculated in separate WQMP report [4]. 2. Hydrologic Data The project site is in San Bernardino County’s Valley Area. Per the NOAA Atlas 14 Point Precipitation Frequency Estimates [5], the 100-year 1-hour, 6-hour, and 24-hour isohyet are 1.65, 4.28, and 8.05 inches, respectively (Appendix C). The slope for rainfall intensity curve is 0.6. The soil group is type A, per the San Bernardino County’s Hydrology Manual [6]. Soil Group A typically has a low runoff potential with high infiltration rate. Antecedent Moisture Condition (AMC) II is used for storm drain system design. The proposed development type is condominium. The curve numbers (CN) for the existing and proposed conditions are 50 and 32, respectively, per San Bernadino County’s Hydrology Manual [6]. 2 3. Methodology San Bernardino County's hydrology methods, available in the software programs of CiviICadd/CivilDesign (Version 7.1) [7], were used for hydrology calculations. Rational Method program was used to calculate Time of Concentration (TC). The hydrograph was calculated using the Unit Hydrograph Method program based on Tc obtained from Rational Method. The detention system routing was calculated by the Flood Hydrograph Routing program, which uses the hydrograph generated from Unit Hydrograph Method. 4. Drainage Analysis 4.1 Existing Condition The site is currently vacant. Based on drainage paths, the onsite runoff flows from high point at northeast area towards the low point at southwest boundary (See Hydrology Map). Tc calculated by Rational method is provided in Appendix D. The results are summarized in Table 1. 4.2 Proposed Condition The proposed onsite drainage is a combination of surface flow, street and gutter flow, catch basin/inlet, and storm drain. Drainage is designed to be discharged to underground chamber systems located at south and southwest of the site. Low flow will be diverted to infiltration chamber while high flow will bypass and be discharged to the detention chamber. Based on drainage pattern, the onsite drainage can be divided into three subareas (see Hydrology Map). Subarea A Runoff from the lots surface flows onto Cascade Drive, then flows westerly along the gutter into a catch basin. Runoff continues southerly through the storm drain on “A” Drive into the diversion structure at southwest corner of the site. Subarea B Runoff from the lots surface flows onto “B” Drive and drains southerly along the gutter into a catch basin and is conveyed to the storm drain. Runoff continues in the storm drain on “C” Drive and flows to the diversion structure. Subarea C 3 Runoff from the lots surface flows onto “C” Drive and drains westerly along the gutter into a catch basin and is conveyed into the storm drain. Runoff continues through the storm drain into the diversion structure. At the diversion structure, low flow is diverted to a concrete box where flow is filtered then conveyed into the infiltration trench. High flow bypasses and drains into the underground detention trench. The detained water is released through an 18” outlet pipe at the rate not exceeding 90% of the existing flow. There is no offsite drainage contributing to the site. Tc calculated by Rational method is provided in Appendix D and summarized in Table 2. Confluence flow calculated by Unit Hydrograph method is provided in Appendix E. 5. Detention Per the hydrology report of Tract No. 17389, the project site is designated for residential development with density of 3-4 units/acre, for which the 100-year peak flow is 20.07 cfs (Appendix B). In current design, the site is proposed for condominium, for which the proposed 100-year peak flow is 28.77 cfs (Appendix D). To mitigate the increased flow, an underground detention system is proposed. Onsite high flow that bypasses the diversion structure drains into the detention system. This system consists of an underground 72” CMP pipe in the trench, with an 18” outlet pipe. The trench is sized to detain the peak flow (Table 3) The slope of the outlet pipe is designed such that maximum of 20.07 cfs can be discharged (Table 4, Appendix F). The detention system’s stage-volume-discharge relation is provided in Table 5. The hydrograph generated from the Unit Hydrograph calculation (Appendix E) was routed through this detention system. The resulted maximum water surface is 6.45’, and the maximum outflow is 20.07 cfs (Table 6, Appendix F). 6. Water Quality Management Plan (WQMP) Per the soil report [8] of the stie, the site has a measured infiltration rate of 15.24 in/hr for projected infiltration locations (Appendix G), which makes infiltration-based CMP feasible. An underground infiltration system with perforated CMP pipes is proposed. A factor of safety of 2.625 is applied to calculate the design infiltration rate [4]. The DCV is 21,232 cf, per the WQMP report [4] (Appendix H). Onsite flow is routed through the storm drain system into the diversion structure, where low flow is filtered via filter insert and discharged into the infiltration trench. This trench consists of four (4) rows of 77’ long 84”-diam perforated CMP pipes in a 79’x39’x8’ trench (Table 7). There is 12” gravel layer placed underneath the pipes, A 3’ depth dirt cover is on the top of the trench. The DCV can be infiltrated in 8.7 hours (Table 8) 4 7. Conclusion The 100-year Tc of the existing and the proposed conditions were calculated for onsite tributary areas using the San Bernardino County Rational Method. The peak flow and hydrograph were calculated using the County’s Unit Hydrograph Method. Flood routing was performed using the County’s Flood Routing Method. Onsite storm drain system including inlets and pipes are proposed to intercept, convey, and discharge onsite runoff. Underground infiltration system is proposed to treat the first flush of stormwater required by WQMP. Another underground detention system is proposed to mitigate the increased peak flow to maintain the allowable outflow designated by the master storm drain plan. Thus, the proposed project does not have negative impacts to the surrounding area. 8. References 1. Hydrology & Hydraulics Report, Tract No. 17389, Allard Engineering, Revised September 6, 2011. 2. Offsite Storm Drain Improvement Plans, Tract No. 17389, City of Fontana, Allard Engineering, November 16, 2011 3. Technical Guidance Document for Water Quality Management Plans, The County of San Bernadino Areawide Stormwater Program, NPDES No. CAS618036, Order No. R8-2010-0036, CDM Smith Inc., June 7, 2013 4. Water Quality Management Plan, Tract No. 20580, United Civil Inc., October 21, 2022 5. https://hdsc.nws.noaa.gov/hdsc/pfds/ 6. San Bernardino County Hydrology Manual, August 1986. 7. CivilDesign Engineering Software, Version 7.1 8. Geologic and Geotechnical Engineering Investigation Report Proposed SFD Residential Development, North Corner of Chase Road & Aria Lane, Fontana, California, Ridge Crest Real Estate, LLC., July 19, 2022. Table 1 – Existing Hydrology Summary Subarea Area Length Soil Group Rain 1-hr 100-YR AMC 100-YR CN (AMC 2) IMP(1) Tc Q100 (2) (ac) (ft) (in) (min) (cfs) A 6.84 837 A 1.65 2 50 0 22.8 14.84 (1)Undeveloped (2)Rational Method Table 2 – Proposed Hydrology Summary Subarea Area Length Soil Group Rain 1-hr 100-YR AMC 100-YR CN (AMC 2) IMP(1) Tc Q100 (2) (ac) (ft) (in) (min) (cfs) A 3.43 1020 A 1.65 2 32 65 10.2 13.74 B 1.79 762 A 1.65 2 32 65 8.6 8.46 C 1.62 456 A 1.65 2 32 65 7.6 7.96 CONF. 6.84 A 1.65 2 32 65 8.6 28.77 (1) Condominium (2) Rational Method Table 3 – Detention System Summary Tributary Area Allowable Q100(1) Proposed Q100 (2) Pipe Length Pipe Diameter # of Rows Trench Length Trench Width Trench Depth Outlet Pipe (ac) (cfs) (cfs) (ft) (in) (ft) (ft) (ft) (in) 6.84 20.07 28.72 92 72 1 94 8 6.5 18 (1) Master SD line (2)Unit Hydrograph Method Table 4 – Detention Outlet Pipe Calculation (D=18”, S=0.0365) Water Depth Outflow (ft) (cfs) 0 0 0.5 4.81 1 15.73 1.5 20.07 Table 5 – Detention System Stage-Volume-Discharge Relation (CMP D=72”, L=92’, Outlet Pipe D=18”) Depth from Trench Bottom Pipe Area Pipe Volume Trench Volume Total Volume Total Volume Q Out (ft) (sf) (cf) (cf) (cf) (ac-ft) (cfs) 0 0 0 0 0 0 0 0.5 0 0 150 150 0.003 0 1 1.1 104 259 363 0.008 4.81 1.5 3.1 285 337 622 0.014 15.73 2 5.5 509 398 907 0.021 20.07 2.5 8.3 759 448 1207 0.028 20.07 3 11.2 1026 492 1518 0.035 20.07 3.5 14.1 1301 532 1833 0.042 20.07 4 17.1 1575 573 2148 0.049 20.07 4.5 20.0 1842 617 2459 0.056 20.07 5 22.8 2093 667 2760 0.063 20.07 5.5 25.2 2317 728 3044 0.070 20.07 6 27.2 2498 806 3303 0.076 20.07 6.5 28.3 2601 915 3516 0.081 20.07 Table 6 – Detention System Routing Site Area Peak Inflow Peak Outflow Maximum Water Depth Drawdown Time (ac) (cfs) (cfs) (ft) (hr) 6.84 28.72 20.07 6.45 8.45 Table 7 – WQMP Infiltration System Summary Site Area DCV (1) Pipe Length Pipe Diameter # of Rows Trench Length Trench Width Depth Below Pipe 3-hr Filling Pipe Volume Trench Volume Total Volume Provided (ac) (cf) (ft) (in) (ft) (ft) (ft) (cf) (cf) (cf) (cf) 6.84 21,232 77 84 4 79 39 1 4,472 11,847 5,120 21,439 (1) See separate WQMP report Table 8 – WQMP Infiltration System Drawdown Calculation Area Retention Volume Infiltration Rate FS Effective Infiltration Average Contact Area Drawdown Time (ac) (cf) (in/hr) (in/hr) (sf) (hr) 6.84 16,968 15.24 2.625 5.81 4,025 8.7 APPENDIX A VICINITY MAP APPENDIX B MASTER STORM DRAIN EXCERPTS (TR NO. 1789) 40 do ALLAFlD ENGINEERING m Boa wmny lana nes gy & Hydraulics 6253 Sierra Ave, Fontana, CA 92335 • (909) 356-1815 • (909) 356-1795 IN MAINLINE TC(MIN.) = 13.08 100 YEAR RAINFALL INTENSITY(INCH/HR) = 3.865 t SUBAREA LOSS RATE DATA(AMC II): IN DEVELOPMENT TYPE/ SCS SOIL AREA Fp Ap SCS LAND USE GROUP (ACRES) (INCH/HR) (DECIMAL) CN No RESIDENTIAL io "3-4 DWELLINGS/ACRE" A 6.80 0.98 0.600 32 SUBAREA AVERAGE PERVIOUS LOSS RATE, Fp(INCH/HR) = 0.98 OK SUBAREA AVERAGE PERVIOUS AREA FRACTION, Ap = 0.600 SUBAREA AREA(ACRES) = 6.80 SUBAREA RUNOFF(CFS) = 20.07 iM EFFECTIVE AREA(ACRES) = 33.84 AREA-AVERAGED Fm(INCH/HR) = 0.53 AREA-AVERAGED Fp(INCH/HR) = 0.97 AREA-AVERAGED Ap = 0.55 am TOTAL AREA(ACRES) = 36.3 PEAK FLOW RATE(CFS) = 101.52 ow w. FLOW PROCESS FROM NODE 1.91 TO NODE 1.91 IS CODE = 81 ADDITION OF SUBAREA TO MAINLINE PEAK FLOW««< MAINLINE Tc(MIN.) = 13.08 to * 100 YEAR RAINFALL INTENSITY(INCH/HR) = 3.865 SUBAREA LOSS RATE DATA(AMC II): DEVELOPMENT TYPE/ SCS SOIL AREA Fp Ap SCS LAND USE GROUP (ACRES) (INCH/HR) (DECIMAL) CN COMMERCIAL A 1.00 0.98 0.100 32 SUBAREA AVERAGE PERVIOUS LOSS RATE, Fp(INCH/HR) = 0.98 SUBAREA AVERAGE PERVIOUS AREA FRACTION, Ap = 0.100 SUBAREA AREA(ACRES) = 1.00 SUBAREA RUNOFF(CFS) = 3.39 EFFECTIVE AREA(ACRES) = 34.84 AREA-AVERAGED Fm(INCH/HR) = 0.52 AREA-AVERAGED Fp(INCH/HR) = 0.97 AREA-AVERAGED Ap = 0.53 TOTAL AREA(ACRES) = 37.3 PEAK FLOW RATE(CFS) = 104.91 am FLOW PROCESS FROM NODE 1.91 TO NODE 1.92 IS CODE = 31 COMPUTE PIPE-FLOW TRAVEL TIME THRU SUBAREA««< USING COMPUTER-ESTIMATED PIPESIZE (NON-PRESSURE FLOW) ««< im ELEVATION DATA: UPSTREAM(FEET) = 1404.70 DOWNSTREAM(FEET) = 1398.70 1rw FLOW LENGTH(FEET) = 420.00 MANNING'S N = 0.013 DEPTH OF FLOW IN 42.0 INCH PIPE IS 32.6 INCHES PIPE-FLOW VELOCITY(FEET/SEC.) = 13.11 ESTIMATED PIPE DIAMETER(INCH) = 42.00 NUMBER OF PIPES = 1 PIPE-FLOW(CFS) = 104.91 PIPE TRAVEL TIME(MIN.) = 0.53 Tc(MIN.) = 13.62 LONGEST FLOWPATH FROM NODE 3.10 TO NODE 1.92 = 3091.00 FEET. FLOW PROCESS FROM NODE 1.92 TO NODE 1.92 IS CODE = 81 AA t------------------------------------------------------- ADDITION OF SUBAREA TO MAINLINE PEAK FLOW««< MAINLINE Tc(MIN.) = 13.62 100 YEAR RAINFALL INTENSITY(INCH/HR) = 3.774 SUBAREA LOSS RATE DATA(AMC II): DEVELOPMENT TYPE/ SCS SOIL AREA Fp Ap SCS LAND USE GROUP (ACRES) (INCH/HR) (DECIMAL) CN 38 0 wr APPENDIX C HYDOLOGIC DATA AND DESIGN CRITERIA 8/11/22, 6:16 PM Precipitation Frequency Data Server https://hdsc.nws.noaa.gov/hdsc/pfds/pfds_printpage.html?lat=34.1258&lon=-117.4570&data=depth&units=english&series=pds 1/4 NOAA Atlas 14, Volume 6, Version 2 Location name: Fontana, California, USA* Latitude: 34.1258°, Longitude: -117.457° Elevation: 1425.11 ft** * source: ESRI Maps ** source: USGS POINT PRECIPITATION FREQUENCY ESTIMATES Sanja Perica, Sarah Dietz, Sarah Heim, Lillian Hiner, Kazungu Maitaria, Deborah Martin, SandraPavlovic, Ishani Roy, Carl Trypaluk, Dale Unruh, Fenglin Yan, Michael Yekta, Tan Zhao, GeoffreyBonnin, Daniel Brewer, Li-Chuan Chen, Tye Parzybok, John Yarchoan NOAA, National Weather Service, Silver Spring, Maryland PF_tabular | PF_graphical | Maps_&_aerials PF tabular PDS-based point precipitation frequency estimates with 90% confidence intervals (in inches)1 Duration Average recurrence interval (years) 1 2 5 10 25 50 100 200 500 1000 5-min 0.127 (0.105‑0.154) 0.167 (0.139‑0.203) 0.221 (0.183‑0.269) 0.265 (0.218‑0.325) 0.325 (0.258‑0.413) 0.372 (0.289‑0.484) 0.421 (0.319‑0.560) 0.471 (0.347‑0.647) 0.542 (0.382‑0.776) 0.598 (0.407‑0.887) 10-min 0.182 (0.151‑0.220) 0.240 (0.199‑0.291) 0.316 (0.262‑0.385) 0.379 (0.312‑0.466) 0.466 (0.370‑0.592) 0.533 (0.415‑0.693) 0.603 (0.457‑0.803) 0.676 (0.498‑0.927) 0.777 (0.548‑1.11) 0.857 (0.584‑1.27) 15-min 0.220 (0.183‑0.266) 0.290 (0.241‑0.352) 0.383 (0.317‑0.466) 0.459 (0.377‑0.564) 0.563 (0.448‑0.716) 0.645 (0.501‑0.838) 0.729 (0.553‑0.971) 0.817 (0.602‑1.12) 0.939 (0.663‑1.35) 1.04 (0.706‑1.54) 30-min 0.329 (0.274‑0.399) 0.434 (0.361‑0.528) 0.573 (0.475‑0.698) 0.687 (0.565‑0.844) 0.844 (0.670‑1.07) 0.966 (0.751‑1.25) 1.09 (0.828‑1.46) 1.22 (0.901‑1.68) 1.41 (0.993‑2.01) 1.55 (1.06‑2.30) 60-min 0.496 (0.413‑0.602) 0.655 (0.545‑0.796) 0.864 (0.717‑1.05) 1.04 (0.852‑1.27) 1.27 (1.01‑1.62) 1.46 (1.13‑1.89) 1.65 (1.25‑2.19) 1.85 (1.36‑2.53) 2.12 (1.50‑3.04) 2.34 (1.60‑3.47) 2-hr 0.760 (0.633‑0.922) 0.993 (0.825‑1.21) 1.29 (1.07‑1.58) 1.54 (1.26‑1.89) 1.87 (1.48‑2.38) 2.12 (1.65‑2.76) 2.38 (1.80‑3.17) 2.64 (1.95‑3.62) 3.00 (2.12‑4.30) 3.29 (2.24‑4.87) 3-hr 0.977 (0.813‑1.19) 1.27 (1.06‑1.54) 1.65 (1.37‑2.01) 1.95 (1.60‑2.40) 2.36 (1.87‑3.00) 2.67 (2.07‑3.46) 2.98 (2.26‑3.97) 3.29 (2.42‑4.52) 3.72 (2.63‑5.33) 4.06 (2.76‑6.02) 6-hr 1.44 (1.20‑1.75) 1.87 (1.56‑2.27) 2.42 (2.00‑2.95) 2.85 (2.34‑3.50) 3.42 (2.72‑4.35) 3.85 (2.99‑5.00) 4.28 (3.24‑5.70) 4.71 (3.47‑6.46) 5.29 (3.73‑7.57) 5.73 (3.90‑8.49) 12-hr 1.96 (1.63‑2.38) 2.56 (2.13‑3.11) 3.30 (2.74‑4.02) 3.89 (3.20‑4.78) 4.65 (3.69‑5.91) 5.21 (4.05‑6.77) 5.77 (4.37‑7.68) 6.32 (4.65‑8.67) 7.05 (4.97‑10.1) 7.59 (5.17‑11.3) 24-hr 2.68 (2.37‑3.09) 3.53 (3.12‑4.07) 4.59 (4.05‑5.31) 5.42 (4.74‑6.32) 6.49 (5.50‑7.82) 7.28 (6.04‑8.96) 8.05 (6.52‑10.1) 8.82 (6.95‑11.4) 9.81 (7.42‑13.2) 10.6 (7.72‑14.7) 2-day 3.27 (2.90‑3.77) 4.41 (3.90‑5.09) 5.85 (5.16‑6.77) 7.00 (6.13‑8.16) 8.52 (7.22‑10.3) 9.66 (8.01‑11.9) 10.8 (8.74‑13.6) 11.9 (9.41‑15.5) 13.5 (10.2‑18.2) 14.6 (10.7‑20.4) 3-day 3.51 (3.11‑4.04) 4.81 (4.25‑5.54) 6.49 (5.72‑7.51) 7.85 (6.87‑9.16) 9.70 (8.22‑11.7) 11.1 (9.23‑13.7) 12.6 (10.2‑15.8) 14.0 (11.1‑18.2) 16.0 (12.1‑21.6) 17.6 (12.9‑24.6) 4-day 3.76 (3.33‑4.33) 5.21 (4.60‑6.01) 7.10 (6.26‑8.21) 8.65 (7.57‑10.1) 10.8 (9.13‑13.0) 12.4 (10.3‑15.3) 14.1 (11.4‑17.8) 15.9 (12.5‑20.6) 18.3 (13.8‑24.7) 20.2 (14.8‑28.2) 7-day 4.30(3.80‑4.95)6.02(5.32‑6.95)8.30(7.32‑9.60)10.2(8.91‑11.9)12.8(10.8‑15.4)14.8(12.3‑18.2)16.9(13.7‑21.3)19.1(15.1‑24.8)22.2(16.8‑29.9)24.6(18.0‑34.3) 10-day 4.65 (4.12‑5.36) 6.56 (5.80‑7.57) 9.11 (8.03‑10.5) 11.2 (9.82‑13.1) 14.2 (12.0‑17.1) 16.5 (13.7‑20.3) 18.9 (15.3‑23.8) 21.4 (16.9‑27.7) 24.9 (18.8‑33.6) 27.7 (20.3‑38.7) 20-day 5.52 (4.89‑6.36) 7.88 (6.96‑9.09) 11.1 (9.75‑12.8) 13.7 (12.0‑16.0) 17.5 (14.8‑21.1) 20.5 (17.0‑25.2) 23.7 (19.2‑29.8) 27.1 (21.3‑35.0) 31.8 (24.1‑42.9) 35.7 (26.1‑49.8) 30-day 6.46 (5.72‑7.44) 9.23 (8.16‑10.6) 13.0 (11.5‑15.0) 16.2 (14.2‑18.9) 20.8 (17.6‑25.0) 24.5 (20.3‑30.1) 28.4 (23.0‑35.7) 32.6 (25.7‑42.2) 38.6 (29.2‑52.0) 43.5 (31.8‑60.7) 45-day 7.71 (6.82‑8.88) 10.9 (9.66‑12.6) 15.4 (13.6‑17.8) 19.2 (16.8‑22.4) 24.6 (20.9‑29.7) 29.1 (24.1‑35.8) 33.9 (27.4‑42.7) 39.0 (30.8‑50.6) 46.5 (35.2‑62.8) 52.7 (38.6‑73.6) 60-day 8.99 (7.96‑10.4) 12.6 (11.1‑14.5) 17.6 (15.5‑20.4) 21.9 (19.2‑25.6) 28.2 (23.9‑34.0) 33.4 (27.7‑41.0) 38.9 (31.5‑49.0) 45.0 (35.5‑58.3) 53.8 (40.7‑72.6) 61.2 (44.8‑85.4) 1 Precipitation frequency (PF) estimates in this table are based on frequency analysis of partial duration series (PDS). Numbers in parenthesis are PF estimates at lower and upper bounds of the 90% confidence interval. The probability that precipitation frequency estimates (for a given duration and average recurrence interval) will be greater than the upper bound (or less than the lower bound) is 5%. Estimates at upper bounds are not checked against probable maximum precipitation (PMP) estimates and may be higher than currently valid PMP values. Please refer to NOAA Atlas 14 document for more information. Back to Top PF graphical 8/11/22, 6:16 PM Precipitation Frequency Data Server https://hdsc.nws.noaa.gov/hdsc/pfds/pfds_printpage.html?lat=34.1258&lon=-117.4570&data=depth&units=english&series=pds 2/4 Back to Top Maps & aerials Small scale terrain 8/11/22, 6:16 PM Precipitation Frequency Data Server https://hdsc.nws.noaa.gov/hdsc/pfds/pfds_printpage.html?lat=34.1258&lon=-117.4570&data=depth&units=english&series=pds 3/4 Large scale terrain Large scale map Large scale aerial + – 3km 2mi + – 100km 60mi + – 100km 60mi 8/11/22, 6:16 PM Precipitation Frequency Data Server https://hdsc.nws.noaa.gov/hdsc/pfds/pfds_printpage.html?lat=34.1258&lon=-117.4570&data=depth&units=english&series=pds 4/4 Back to Top US Department of Commerce National Oceanic and Atmospheric Administration National Weather Service National Water Center 1325 East West Highway Silver Spring, MD 20910 Questions?: HDSC.Questions@noaa.gov Disclaimer + – 100km 60mi Technical Guidance Document for Water Quality Management Plans Prepared by: CDM Smith Inc. Prepared for and Submitted by: The County of San Bernardino Areawide Stormwater Program NPDES No. CAS618036, ORDER No. R8-2010-0036 Submitted To: California Water Quality Control Board – Santa Ana Region June 7, 2013 Approval Date: June 21, 2013 Effective Date: September 19, 2013 64 While conventional pavement results in increased rates and volumes of stormwater and non- stormwater runoff, properly constructed and maintained porous pavement BMPs allow stormwater to percolate through the pavement and enter the soil below. This facilitates groundwater recharge while providing the structural and functional features needed for the roadway, parking lot, or sidewalk. The paving surface, subgrade, and installation requirements of permeable pavements are more complex than those for conventional asphalt or concrete surfaces. For permeable pavement BMPs to function properly over an expected life span of 15 to 20 years, they must be properly sited, carefully designed and installed, and periodically maintained. Failure to protect paved areas from construction-related sediment loads can result in their premature clogging and failure. Retention volume provided by permeable pavement is a function of the infiltrating surface area into underlying soils and the depth of water that is either percolated over the course of the storm or stored within the BMP for percolation into soils following the storm (Table 5-4). Volume retention is estimated using the same equation as used for drywells and undergound infiltration. 5.4.2.6 Underground Infiltration Underground infiltration BMPs typically include a vault or chamber with an open bottom that is used to store runoff and infiltrate the runoff into the subsurface soils and aquifer. A number of vendors offer proprietary products that allow for similar or enhanced rates of infiltration and subsurface storage while offering durable prefabricated structures. There are many varieties of proprietary infiltration BMPs that can be used for roads and parking lots, parks and open spaces, single and multi-family residential, or mixed-use and commercial uses. Retention volume provided by underground infiltration is a function of the surface area infiltrating into underlying soils and the depth of water that is either percolated over the course of the storm or stored within the BMP for percolation into soils following the storm (Table 5-4). Volume retention is estimated using the same equation as used for drywells and permeable pavement. 5.4.3 Harvest and Use BMPs Harvest and use BMPs are BMPs that capture and store stormwater runoff for later on-site use. These BMPs are engineered to store a specified volume of water and have no design surface discharge until this volume is exceeded. The use of captured water used should comply with codes and regulations and should not result in runoff to storm drains or receiving waters (except indirectly via the sanitary sewer/municipal wastewater treatment system). Uses of captured water may potentially include irrigation demand, indoor non-potable demand, industrial process water demand, or other demands. This document provides guidance for irrigation use. Use of harvested stormwater for other non-potable demands shall be evaluated APPENDIX D RATIONAL METHOD CALCULATION EXISTING CONDITION San Bernardino County Rational Hydrology Program (Hydrology Manual Date ‐ August 1986) CIVILCADD/CIVILDESIGN Engineering Software, (c) 1989‐2018 Version 9.0 Rational Hydrology Study Date: 08/03/22 ‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐ Program License Serial Number 6427 ‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐ ********* Hydrology Study Control Information ********** ‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐ Rational hydrology study storm event year is 100.0 Computed rainfall intensity: Storm year = 100.00 1 hour rainfall = 1.650 (In.) Slope used for rainfall intensity curve b = 0.6000 Soil antecedent moisture condition (AMC) = 3 ++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ Process from Point/Station 100.000 to Point/Station 110.000 **** INITIAL AREA EVALUATION **** ______________________________________________________________________ UNDEVELOPED (average cover) subarea Decimal fraction soil group A = 1.000 Decimal fraction soil group B = 0.000 Decimal fraction soil group C = 0.000 Decimal fraction soil group D = 0.000 SCS curve number for soil(AMC 2) = 50.00 Adjusted SCS curve number for AMC 3 = 70.00 Pervious ratio(Ap) = 1.0000 Max loss rate(Fm)= 0.532(In/Hr) Initial subarea data: Initial area flow distance = 837.100(Ft.) Top (of initial area) elevation = 1430.100(Ft.) Bottom (of initial area) elevation = 1413.470(Ft.) Difference in elevation = 16.630(Ft.) Slope = 0.01987 s(%)= 1.99 TC = k(0.706)*[(length^3)/(elevation change)]^0.2 Initial area time of concentration = 22.819 min. Rainfall intensity = 2.947(In/Hr) for a 100.0 year storm Effective runoff coefficient used for area (Q=KCIA) is C = 0.737 Subarea runoff = 14.843(CFS) Total initial stream area = 6.830(Ac.) Pervious area fraction = 1.000 Initial area Fm value = 0.532(In/Hr) End of computations, Total Study Area = 6.83 (Ac.) The following figures may be used for a unit hydrograph study of the same area. Note: These figures do not consider reduced effective area effects caused by confluences in the rational equation. Area averaged pervious area fraction(Ap) = 1.000 Area averaged SCS curve number = 50.0 PROPOSED CONDITION San Bernardino County Rational Hydrology Program (Hydrology Manual Date ‐ August 1986) CIVILCADD/CIVILDESIGN Engineering Software, (c) 1989‐2018 Version 9.0 Rational Hydrology Study Date: 12/01/22 ‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐ Program License Serial Number 6427 ‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐ ********* Hydrology Study Control Information ********** ‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐ Rational hydrology study storm event year is 100.0 Computed rainfall intensity: Storm year = 100.00 1 hour rainfall = 1.650 (In.) Slope used for rainfall intensity curve b = 0.6000 Soil antecedent moisture condition (AMC) = 2 ++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ Process from Point/Station 100.000 to Point/Station 110.000 **** INITIAL AREA EVALUATION **** ______________________________________________________________________ CONDOMINIUM subarea type Decimal fraction soil group A = 1.000 Decimal fraction soil group B = 0.000 Decimal fraction soil group C = 0.000 Decimal fraction soil group D = 0.000 SCS curve number for soil(AMC 2) = 32.00 Pervious ratio(Ap) = 0.3500 Max loss rate(Fm)= 0.342(In/Hr) Initial subarea data: Initial area flow distance = 107.000(Ft.) Top (of initial area) elevation = 1429.700(Ft.) Bottom (of initial area) elevation = 1427.400(Ft.) Difference in elevation = 2.300(Ft.) Slope = 0.02150 s(%)= 2.15 TC = k(0.360)*[(length^3)/(elevation change)]^0.2 Initial area time of concentration = 5.030 min. Rainfall intensity = 7.302(In/Hr) for a 100.0 year storm Effective runoff coefficient used for area (Q=KCIA) is C = 0.858 Subarea runoff = 1.253(CFS) Total initial stream area = 0.200(Ac.) Pervious area fraction = 0.350 Initial area Fm value = 0.342(In/Hr) ++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ Process from Point/Station 110.000 to Point/Station 120.000 **** STREET FLOW TRAVEL TIME + SUBAREA FLOW ADDITION **** ______________________________________________________________________ Top of street segment elevation = 1427.400(Ft.) End of street segment elevation = 1425.700(Ft.) Length of street segment = 379.000(Ft.) Height of curb above gutter flowline = 6.0(In.) Width of half street (curb to crown) = 20.000(Ft.) Distance from crown to crossfall grade break = 18.000(Ft.) Slope from gutter to grade break (v/hz) = 0.080 Slope from grade break to crown (v/hz) = 0.020 Street flow is on [2] side(s) of the street Distance from curb to property line = 10.000(Ft.) Slope from curb to property line (v/hz) = 0.020 Gutter width = 2.000(Ft.) Gutter hike from flowline = 2.000(In.) Manning's N in gutter = 0.0150 Manning's N from gutter to grade break = 0.0150 Manning's N from grade break to crown = 0.0150 Estimated mean flow rate at midpoint of street = 4.166(CFS) Depth of flow = 0.345(Ft.), Average velocity = 1.585(Ft/s) Streetflow hydraulics at midpoint of street travel: Halfstreet flow width = 10.896(Ft.) Flow velocity = 1.59(Ft/s) Travel time = 3.98 min. TC = 9.01 min. Adding area flow to street CONDOMINIUM subarea type Decimal fraction soil group A = 1.000 Decimal fraction soil group B = 0.000 Decimal fraction soil group C = 0.000 Decimal fraction soil group D = 0.000 SCS curve number for soil(AMC 2) = 32.00 Pervious ratio(Ap) = 0.3500 Max loss rate(Fm)= 0.342(In/Hr) Rainfall intensity = 5.145(In/Hr) for a 100.0 year storm Effective runoff coefficient used for area,(total area with modified rational method)(Q=KCIA) is C = 0.840 Subarea runoff = 5.707(CFS) for 1.410(Ac.) Total runoff = 6.960(CFS) Effective area this stream = 1.61(Ac.) Total Study Area (Main Stream No. 1) = 1.61(Ac.) Area averaged Fm value = 0.342(In/Hr) Street flow at end of street = 6.960(CFS) Half street flow at end of street = 3.480(CFS) Depth of flow = 0.396(Ft.), Average velocity = 1.789(Ft/s) Flow width (from curb towards crown)= 13.484(Ft.) ++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ Process from Point/Station 120.000 to Point/Station 130.000 **** PIPEFLOW TRAVEL TIME (User specified size) **** ______________________________________________________________________ Upstream point/station elevation = 1425.700(Ft.) Downstream point/station elevation = 1416.000(Ft.) Pipe length = 534.00(Ft.) Manning's N = 0.013 No. of pipes = 1 Required pipe flow = 6.960(CFS) Given pipe size = 24.00(In.) Calculated individual pipe flow = 6.960(CFS) Normal flow depth in pipe = 7.79(In.) Flow top width inside pipe = 22.48(In.) Critical Depth = 11.23(In.) Pipe flow velocity = 7.86(Ft/s) Travel time through pipe = 1.13 min. Time of concentration (TC) = 10.15 min. ++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ Process from Point/Station 140.000 to Point/Station 130.000 **** SUBAREA FLOW ADDITION **** ______________________________________________________________________ CONDOMINIUM subarea type Decimal fraction soil group A = 1.000 Decimal fraction soil group B = 0.000 Decimal fraction soil group C = 0.000 Decimal fraction soil group D = 0.000 SCS curve number for soil(AMC 2) = 32.00 Pervious ratio(Ap) = 0.3500 Max loss rate(Fm)= 0.342(In/Hr) Time of concentration = 10.15 min. Rainfall intensity = 4.793(In/Hr) for a 100.0 year storm Effective runoff coefficient used for area,(total area with modified rational method)(Q=KCIA) is C = 0.836 Subarea runoff = 6.779(CFS) for 1.820(Ac.) Total runoff = 13.739(CFS) Effective area this stream = 3.43(Ac.) Total Study Area (Main Stream No. 1) = 3.43(Ac.) Area averaged Fm value = 0.342(In/Hr) End of computations, Total Study Area = 3.43 (Ac.) The following figures may be used for a unit hydrograph study of the same area. Note: These figures do not consider reduced effective area effects caused by confluences in the rational equation. Area averaged pervious area fraction(Ap) = 0.350 Area averaged SCS curve number = 32.0 San Bernardino County Rational Hydrology Program (Hydrology Manual Date ‐ August 1986) CIVILCADD/CIVILDESIGN Engineering Software, (c) 1989‐2018 Version 9.0 Rational Hydrology Study Date: 12/01/22 ‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐ Program License Serial Number 6427 ‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐ ********* Hydrology Study Control Information ********** ‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐ Rational hydrology study storm event year is 100.0 Computed rainfall intensity: Storm year = 100.00 1 hour rainfall = 1.650 (In.) Slope used for rainfall intensity curve b = 0.6000 Soil antecedent moisture condition (AMC) = 2 ++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ Process from Point/Station 200.000 to Point/Station 210.000 **** INITIAL AREA EVALUATION **** ______________________________________________________________________ CONDOMINIUM subarea type Decimal fraction soil group A = 1.000 Decimal fraction soil group B = 0.000 Decimal fraction soil group C = 0.000 Decimal fraction soil group D = 0.000 SCS curve number for soil(AMC 2) = 32.00 Pervious ratio(Ap) = 0.3500 Max loss rate(Fm)= 0.342(In/Hr) Initial subarea data: Initial area flow distance = 120.200(Ft.) Top (of initial area) elevation = 1427.800(Ft.) Bottom (of initial area) elevation = 1426.500(Ft.) Difference in elevation = 1.300(Ft.) Slope = 0.01082 s(%)= 1.08 TC = k(0.360)*[(length^3)/(elevation change)]^0.2 Initial area time of concentration = 6.046 min. Rainfall intensity = 6.539(In/Hr) for a 100.0 year storm Effective runoff coefficient used for area (Q=KCIA) is C = 0.853 Subarea runoff = 1.115(CFS) Total initial stream area = 0.200(Ac.) Pervious area fraction = 0.350 Initial area Fm value = 0.342(In/Hr) ++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ Process from Point/Station 210.000 to Point/Station 220.000 **** STREET FLOW TRAVEL TIME + SUBAREA FLOW ADDITION **** ______________________________________________________________________ Top of street segment elevation = 1426.500(Ft.) End of street segment elevation = 1418.800(Ft.) Length of street segment = 333.000(Ft.) Height of curb above gutter flowline = 6.0(In.) Width of half street (curb to crown) = 20.000(Ft.) Distance from crown to crossfall grade break = 18.000(Ft.) Slope from gutter to grade break (v/hz) = 0.080 Slope from grade break to crown (v/hz) = 0.020 Street flow is on [2] side(s) of the street Distance from curb to property line = 10.000(Ft.) Slope from curb to property line (v/hz) = 0.020 Gutter width = 2.000(Ft.) Gutter hike from flowline = 2.000(In.) Manning's N in gutter = 0.0150 Manning's N from gutter to grade break = 0.0150 Manning's N from grade break to crown = 0.0150 Estimated mean flow rate at midpoint of street = 4.841(CFS) Depth of flow = 0.289(Ft.), Average velocity = 3.096(Ft/s) Streetflow hydraulics at midpoint of street travel: Halfstreet flow width = 8.094(Ft.) Flow velocity = 3.10(Ft/s) Travel time = 1.79 min. TC = 7.84 min. Adding area flow to street CONDOMINIUM subarea type Decimal fraction soil group A = 1.000 Decimal fraction soil group B = 0.000 Decimal fraction soil group C = 0.000 Decimal fraction soil group D = 0.000 SCS curve number for soil(AMC 2) = 32.00 Pervious ratio(Ap) = 0.3500 Max loss rate(Fm)= 0.342(In/Hr) Rainfall intensity = 5.595(In/Hr) for a 100.0 year storm Effective runoff coefficient used for area,(total area with modified rational method)(Q=KCIA) is C = 0.845 Subarea runoff = 7.348(CFS) for 1.590(Ac.) Total runoff = 8.463(CFS) Effective area this stream = 1.79(Ac.) Total Study Area (Main Stream No. 1) = 1.79(Ac.) Area averaged Fm value = 0.342(In/Hr) Street flow at end of street = 8.463(CFS) Half street flow at end of street = 4.231(CFS) Depth of flow = 0.334(Ft.), Average velocity = 3.508(Ft/s) Flow width (from curb towards crown)= 10.390(Ft.) ++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ Process from Point/Station 220.000 to Point/Station 130.000 **** PIPEFLOW TRAVEL TIME (User specified size) **** ______________________________________________________________________ Upstream point/station elevation = 1418.800(Ft.) Downstream point/station elevation = 1416.000(Ft.) Pipe length = 309.00(Ft.) Manning's N = 0.013 No. of pipes = 1 Required pipe flow = 8.463(CFS) Given pipe size = 24.00(In.) Calculated individual pipe flow = 8.463(CFS) Normal flow depth in pipe = 10.45(In.) Flow top width inside pipe = 23.80(In.) Critical Depth = 12.43(In.) Pipe flow velocity = 6.44(Ft/s) Travel time through pipe = 0.80 min. Time of concentration (TC) = 8.64 min. End of computations, Total Study Area = 1.79 (Ac.) The following figures may be used for a unit hydrograph study of the same area. Note: These figures do not consider reduced effective area effects caused by confluences in the rational equation. Area averaged pervious area fraction(Ap) = 0.350 Area averaged SCS curve number = 32.0 San Bernardino County Rational Hydrology Program (Hydrology Manual Date ‐ August 1986) CIVILCADD/CIVILDESIGN Engineering Software, (c) 1989‐2018 Version 9.0 Rational Hydrology Study Date: 12/01/22 ‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐ Program License Serial Number 6427 ‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐ ********* Hydrology Study Control Information ********** ‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐ Rational hydrology study storm event year is 100.0 Computed rainfall intensity: Storm year = 100.00 1 hour rainfall = 1.650 (In.) Slope used for rainfall intensity curve b = 0.6000 Soil antecedent moisture condition (AMC) = 2 ++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ Process from Point/Station 300.000 to Point/Station 310.000 **** INITIAL AREA EVALUATION **** ______________________________________________________________________ CONDOMINIUM subarea type Decimal fraction soil group A = 1.000 Decimal fraction soil group B = 0.000 Decimal fraction soil group C = 0.000 Decimal fraction soil group D = 0.000 SCS curve number for soil(AMC 2) = 32.00 Pervious ratio(Ap) = 0.3500 Max loss rate(Fm)= 0.342(In/Hr) Initial subarea data: Initial area flow distance = 67.200(Ft.) Top (of initial area) elevation = 1420.100(Ft.) Bottom (of initial area) elevation = 1419.500(Ft.) Difference in elevation = 0.600(Ft.) Slope = 0.00893 s(%)= 0.89 TC = k(0.360)*[(length^3)/(elevation change)]^0.2 Initial area time of concentration = 4.978 min. Rainfall intensity = 7.347(In/Hr) for a 100.0 year storm Effective runoff coefficient used for area (Q=KCIA) is C = 0.858 Subarea runoff = 1.261(CFS) Total initial stream area = 0.200(Ac.) Pervious area fraction = 0.350 Initial area Fm value = 0.342(In/Hr) ++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ Process from Point/Station 310.000 to Point/Station 340.000 **** STREET FLOW TRAVEL TIME + SUBAREA FLOW ADDITION **** ______________________________________________________________________ Top of street segment elevation = 1419.500(Ft.) End of street segment elevation = 1417.000(Ft.) Length of street segment = 299.000(Ft.) Height of curb above gutter flowline = 6.0(In.) Width of half street (curb to crown) = 20.000(Ft.) Distance from crown to crossfall grade break = 18.000(Ft.) Slope from gutter to grade break (v/hz) = 0.080 Slope from grade break to crown (v/hz) = 0.020 Street flow is on [2] side(s) of the street Distance from curb to property line = 10.000(Ft.) Slope from curb to property line (v/hz) = 0.020 Gutter width = 2.000(Ft.) Gutter hike from flowline = 2.000(In.) Manning's N in gutter = 0.0150 Manning's N from gutter to grade break = 0.0150 Manning's N from grade break to crown = 0.0150 Estimated mean flow rate at midpoint of street = 4.687(CFS) Depth of flow = 0.327(Ft.), Average velocity = 2.070(Ft/s) Streetflow hydraulics at midpoint of street travel: Halfstreet flow width = 10.027(Ft.) Flow velocity = 2.07(Ft/s) Travel time = 2.41 min. TC = 7.39 min. Adding area flow to street CONDOMINIUM subarea type Decimal fraction soil group A = 1.000 Decimal fraction soil group B = 0.000 Decimal fraction soil group C = 0.000 Decimal fraction soil group D = 0.000 SCS curve number for soil(AMC 2) = 32.00 Pervious ratio(Ap) = 0.3500 Max loss rate(Fm)= 0.342(In/Hr) Rainfall intensity = 5.799(In/Hr) for a 100.0 year storm Effective runoff coefficient used for area,(total area with modified rational method)(Q=KCIA) is C = 0.847 Subarea runoff = 6.695(CFS) for 1.420(Ac.) Total runoff = 7.956(CFS) Effective area this stream = 1.62(Ac.) Total Study Area (Main Stream No. 1) = 1.62(Ac.) Area averaged Fm value = 0.342(In/Hr) Street flow at end of street = 7.956(CFS) Half street flow at end of street = 3.978(CFS) Depth of flow = 0.377(Ft.), Average velocity = 2.342(Ft/s) Flow width (from curb towards crown)= 12.538(Ft.) ++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ Process from Point/Station 340.000 to Point/Station 130.000 **** PIPEFLOW TRAVEL TIME (User specified size) **** ______________________________________________________________________ Upstream point/station elevation = 417.000(Ft.) Downstream point/station elevation = 416.000(Ft.) Pipe length = 90.00(Ft.) Manning's N = 0.013 No. of pipes = 1 Required pipe flow = 7.956(CFS) Given pipe size = 24.00(In.) Calculated individual pipe flow = 7.956(CFS) Normal flow depth in pipe = 9.55(In.) Flow top width inside pipe = 23.49(In.) Critical Depth = 12.06(In.) Pipe flow velocity = 6.83(Ft/s) Travel time through pipe = 0.22 min. Time of concentration (TC) = 7.61 min. End of computations, Total Study Area = 1.62 (Ac.) The following figures may be used for a unit hydrograph study of the same area. Note: These figures do not consider reduced effective area effects caused by confluences in the rational equation. Area averaged pervious area fraction(Ap) = 0.350 Area averaged SCS curve number = 32.0 San Bernardino County Rational Hydrology Program (Hydrology Manual Date ‐ August 1986) CIVILCADD/CIVILDESIGN Engineering Software, (c) 1989‐2018 Version 9.0 Rational Hydrology Study Date: 12/01/22 ‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐ Program License Serial Number 6427 ‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐ ********* Hydrology Study Control Information ********** ‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐ Rational hydrology study storm event year is 100.0 Computed rainfall intensity: Storm year = 100.00 1 hour rainfall = 1.650 (In.) Slope used for rainfall intensity curve b = 0.6000 Soil antecedent moisture condition (AMC) = 2 ++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ Process from Point/Station 100.000 to Point/Station 130.000 **** USER DEFINED FLOW INFORMATION AT A POINT **** ______________________________________________________________________ CONDOMINIUM subarea type Decimal fraction soil group A = 1.000 Decimal fraction soil group B = 0.000 Decimal fraction soil group C = 0.000 Decimal fraction soil group D = 0.000 SCS curve number for soil(AMC 2) = 32.00 Pervious ratio(Ap) = 0.3500 Max loss rate(Fm)= 0.342(In/Hr) Rainfall intensity = 4.792(In/Hr) for a 100.0 year storm User specified values are as follows: TC = 10.15 min. Rain intensity = 4.79(In/Hr) Total area this stream = 3.43(Ac.) Total Study Area (Main Stream No. 1) = 3.43(Ac.) Total runoff = 13.74(CFS) ++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ Process from Point/Station 100.000 to Point/Station 130.000 **** CONFLUENCE OF MINOR STREAMS **** ______________________________________________________________________ Along Main Stream number: 1 in normal stream number 1 Stream flow area = 3.430(Ac.) Runoff from this stream = 13.740(CFS) Time of concentration = 10.15 min. Rainfall intensity = 4.792(In/Hr) Area averaged loss rate (Fm) = 0.3422(In/Hr) Area averaged Pervious ratio (Ap) = 0.3500 ++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ Process from Point/Station 200.000 to Point/Station 130.000 **** USER DEFINED FLOW INFORMATION AT A POINT **** ______________________________________________________________________ CONDOMINIUM subarea type Decimal fraction soil group A = 1.000 Decimal fraction soil group B = 0.000 Decimal fraction soil group C = 0.000 Decimal fraction soil group D = 0.000 SCS curve number for soil(AMC 2) = 32.00 Pervious ratio(Ap) = 0.3500 Max loss rate(Fm)= 0.342(In/Hr) Rainfall intensity = 5.278(In/Hr) for a 100.0 year storm User specified values are as follows: TC = 8.64 min. Rain intensity = 5.28(In/Hr) Total area this stream = 1.79(Ac.) Total Study Area (Main Stream No. 1) = 5.22(Ac.) Total runoff = 8.46(CFS) ++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ Process from Point/Station 200.000 to Point/Station 130.000 **** CONFLUENCE OF MINOR STREAMS **** ______________________________________________________________________ Along Main Stream number: 1 in normal stream number 2 Stream flow area = 1.790(Ac.) Runoff from this stream = 8.460(CFS) Time of concentration = 8.64 min. Rainfall intensity = 5.278(In/Hr) Area averaged loss rate (Fm) = 0.3422(In/Hr) Area averaged Pervious ratio (Ap) = 0.3500 ++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ Process from Point/Station 300.000 to Point/Station 130.000 **** USER DEFINED FLOW INFORMATION AT A POINT **** ______________________________________________________________________ CONDOMINIUM subarea type Decimal fraction soil group A = 1.000 Decimal fraction soil group B = 0.000 Decimal fraction soil group C = 0.000 Decimal fraction soil group D = 0.000 SCS curve number for soil(AMC 2) = 32.00 Pervious ratio(Ap) = 0.3500 Max loss rate(Fm)= 0.342(In/Hr) Rainfall intensity = 5.696(In/Hr) for a 100.0 year storm User specified values are as follows: TC = 7.61 min. Rain intensity = 5.70(In/Hr) Total area this stream = 1.62(Ac.) Total Study Area (Main Stream No. 1) = 6.84(Ac.) Total runoff = 7.96(CFS) ++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ Process from Point/Station 300.000 to Point/Station 130.000 **** CONFLUENCE OF MINOR STREAMS **** ______________________________________________________________________ Along Main Stream number: 1 in normal stream number 3 Stream flow area = 1.620(Ac.) Runoff from this stream = 7.960(CFS) Time of concentration = 7.61 min. Rainfall intensity = 5.696(In/Hr) Area averaged loss rate (Fm) = 0.3422(In/Hr) Area averaged Pervious ratio (Ap) = 0.3500 Summary of stream data: Stream Flow rate Area TC Fm Rainfall Intensity No. (CFS) (Ac.) (min) (In/Hr) (In/Hr) 1 13.74 3.430 10.15 0.342 4.792 2 8.46 1.790 8.64 0.342 5.278 3 7.96 1.620 7.61 0.342 5.696 Qmax(1) = 1.000 * 1.000 * 13.740) + 0.901 * 1.000 * 8.460) + 0.831 * 1.000 * 7.960) + = 27.983 Qmax(2) = 1.109 * 0.851 * 13.740) + 1.000 * 1.000 * 8.460) + 0.922 * 1.000 * 7.960) + = 28.773 Qmax(3) = 1.203 * 0.750 * 13.740) + 1.085 * 0.881 * 8.460) + 1.000 * 1.000 * 7.960) + = 28.436 Total of 3 streams to confluence: Flow rates before confluence point: 13.740 8.460 7.960 Maximum flow rates at confluence using above data: 27.983 28.773 28.436 Area of streams before confluence: 3.430 1.790 1.620 Effective area values after confluence: 6.840 6.330 5.768 Results of confluence: Total flow rate = 28.773(CFS) Time of concentration = 8.640 min. Effective stream area after confluence = 6.330(Ac.) Study area average Pervious fraction(Ap) = 0.350 Study area average soil loss rate(Fm) = 0.342(In/Hr) Study area total (this main stream) = 6.84(Ac.) End of computations, Total Study Area = 6.84 (Ac.) The following figures may be used for a unit hydrograph study of the same area. Note: These figures do not consider reduced effective area effects caused by confluences in the rational equation. Area averaged pervious area fraction(Ap) = 0.350 Area averaged SCS curve number = 32.0 APPENDIX E UNIT HYDROGRAPH CALCULATION EXISTING CONDITION U n i t H y d r o g r a p h A n a l y s i s Copyright (c) CIVILCADD/CIVILDESIGN, 1989 ‐ 2018, Version 9.0 Study date 08/08/22 ++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ ‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐ San Bernardino County Synthetic Unit Hydrology Method Manual date ‐ August 1986 Program License Serial Number 6427 ‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐ ‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐ Storm Event Year = 100 Antecedent Moisture Condition = 3 English (in‐lb) Input Units Used English Rainfall Data (Inches) Input Values Used English Units used in output format Area averaged rainfall intensity isohyetal data: Sub‐Area Duration Isohyetal (Ac.) (hours) (In) Rainfall data for year 100 6.84 1 1.65 ‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐ Rainfall data for year 100 6.84 6 4.28 ‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐ Rainfall data for year 100 6.84 24 8.05 ‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐ ++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ ******** Area‐averaged max loss rate, Fm ******** SCS curve SCS curve Area Area Fp(Fig C6) Ap Fm No.(AMCII) NO.(AMC 3) (Ac.) Fraction (In/Hr) (dec.) (In/Hr) 50.0 70.0 6.84 1.000 0.532 1.000 0.532 Area‐averaged adjusted loss rate Fm (In/Hr) = 0.532 ********* Area‐Averaged low loss rate fraction, Yb ********** Area Area SCS CN SCS CN S Pervious (Ac.) Fract (AMC2) (AMC3) Yield Fr 6.84 1.000 50.0 70.0 4.29 0.560 Area‐averaged catchment yield fraction, Y = 0.560 Area‐averaged low loss fraction, Yb = 0.440 User entry of time of concentration = 0.380 (hours) ++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ Watershed area = 6.84(Ac.) Catchment Lag time = 0.304 hours Unit interval = 5.000 minutes Unit interval percentage of lag time = 27.4123 Hydrograph baseflow = 0.00(CFS) Average maximum watershed loss rate(Fm) = 0.532(In/Hr) Average low loss rate fraction (Yb) = 0.440 (decimal) VALLEY UNDEVELOPED S‐Graph Selected Computed peak 5‐minute rainfall = 0.611(In) Computed peak 30‐minute rainfall = 1.250(In) Specified peak 1‐hour rainfall = 1.650(In) Computed peak 3‐hour rainfall = 2.960(In) Specified peak 6‐hour rainfall = 4.280(In) Specified peak 24‐hour rainfall = 8.050(In) Rainfall depth area reduction factors: Using a total area of 6.84(Ac.) (Ref: fig. E‐4) 5‐minute factor = 1.000 Adjusted rainfall = 0.610(In) 30‐minute factor = 1.000 Adjusted rainfall = 1.250(In) 1‐hour factor = 1.000 Adjusted rainfall = 1.649(In) 3‐hour factor = 1.000 Adjusted rainfall = 2.960(In) 6‐hour factor = 1.000 Adjusted rainfall = 4.280(In) 24‐hour factor = 1.000 Adjusted rainfall = 8.050(In) ‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐ U n i t H y d r o g r a p h +++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ Interval 'S' Graph Unit Hydrograph Number Mean values ((CFS)) ‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐ (K = 82.72 (CFS)) 1 2.576 2.131 2 11.593 7.459 3 27.617 13.255 4 46.751 15.828 5 61.026 11.809 6 69.457 6.975 7 74.726 4.358 8 78.637 3.236 9 81.789 2.607 10 84.414 2.172 11 86.623 1.827 12 88.414 1.482 13 90.047 1.351 14 91.383 1.105 15 92.562 0.975 16 93.496 0.773 17 94.364 0.718 18 95.191 0.684 19 95.950 0.628 20 96.560 0.504 21 97.115 0.459 22 97.608 0.408 23 98.035 0.353 24 98.414 0.314 25 98.716 0.250 26 98.990 0.227 27 99.264 0.227 28 99.538 0.227 29 99.813 0.227 30 100.000 0.155 ‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐ Peak Unit Adjusted mass rainfall Unit rainfall Number (In) (In) 1 0.6105 0.6105 2 0.8055 0.1951 3 0.9474 0.1418 4 1.0629 0.1155 5 1.1621 0.0992 6 1.2501 0.0879 7 1.3296 0.0795 8 1.4025 0.0729 9 1.4702 0.0677 10 1.5335 0.0633 11 1.5930 0.0596 12 1.6495 0.0564 13 1.7213 0.0718 14 1.7905 0.0692 15 1.8575 0.0670 16 1.9224 0.0649 17 1.9854 0.0630 18 2.0468 0.0613 19 2.1065 0.0598 20 2.1648 0.0583 21 2.2218 0.0570 22 2.2775 0.0557 23 2.3320 0.0545 24 2.3854 0.0534 25 2.4378 0.0524 26 2.4892 0.0514 27 2.5397 0.0505 28 2.5894 0.0496 29 2.6382 0.0488 30 2.6862 0.0480 31 2.7335 0.0473 32 2.7801 0.0466 33 2.8260 0.0459 34 2.8713 0.0453 35 2.9159 0.0446 36 2.9600 0.0440 37 3.0034 0.0435 38 3.0463 0.0429 39 3.0887 0.0424 40 3.1306 0.0419 41 3.1720 0.0414 42 3.2129 0.0409 43 3.2534 0.0405 44 3.2934 0.0400 45 3.3330 0.0396 46 3.3722 0.0392 47 3.4111 0.0388 48 3.4495 0.0384 49 3.4875 0.0380 50 3.5252 0.0377 51 3.5625 0.0373 52 3.5995 0.0370 53 3.6362 0.0367 54 3.6725 0.0363 55 3.7086 0.0360 56 3.7443 0.0357 57 3.7797 0.0354 58 3.8148 0.0351 59 3.8497 0.0349 60 3.8843 0.0346 61 3.9186 0.0343 62 3.9526 0.0340 63 3.9864 0.0338 64 4.0200 0.0335 65 4.0532 0.0333 66 4.0863 0.0331 67 4.1191 0.0328 68 4.1517 0.0326 69 4.1841 0.0324 70 4.2162 0.0322 71 4.2482 0.0319 72 4.2799 0.0317 73 4.3069 0.0270 74 4.3337 0.0268 75 4.3603 0.0266 76 4.3867 0.0264 77 4.4129 0.0262 78 4.4389 0.0260 79 4.4647 0.0258 80 4.4904 0.0257 81 4.5159 0.0255 82 4.5412 0.0253 83 4.5664 0.0252 84 4.5914 0.0250 85 4.6162 0.0248 86 4.6409 0.0247 87 4.6654 0.0245 88 4.6897 0.0244 89 4.7139 0.0242 90 4.7380 0.0241 91 4.7619 0.0239 92 4.7857 0.0238 93 4.8093 0.0236 94 4.8328 0.0235 95 4.8562 0.0234 96 4.8794 0.0232 97 4.9025 0.0231 98 4.9255 0.0230 99 4.9483 0.0228 100 4.9710 0.0227 101 4.9936 0.0226 102 5.0161 0.0225 103 5.0385 0.0224 104 5.0607 0.0222 105 5.0828 0.0221 106 5.1048 0.0220 107 5.1267 0.0219 108 5.1485 0.0218 109 5.1701 0.0217 110 5.1917 0.0216 111 5.2132 0.0215 112 5.2345 0.0213 113 5.2558 0.0212 114 5.2769 0.0211 115 5.2979 0.0210 116 5.3189 0.0209 117 5.3397 0.0208 118 5.3605 0.0207 119 5.3811 0.0207 120 5.4017 0.0206 121 5.4222 0.0205 122 5.4425 0.0204 123 5.4628 0.0203 124 5.4830 0.0202 125 5.5031 0.0201 126 5.5231 0.0200 127 5.5431 0.0199 128 5.5629 0.0198 129 5.5827 0.0198 130 5.6024 0.0197 131 5.6220 0.0196 132 5.6415 0.0195 133 5.6609 0.0194 134 5.6803 0.0194 135 5.6996 0.0193 136 5.7188 0.0192 137 5.7379 0.0191 138 5.7569 0.0190 139 5.7759 0.0190 140 5.7948 0.0189 141 5.8136 0.0188 142 5.8324 0.0188 143 5.8511 0.0187 144 5.8697 0.0186 145 5.8882 0.0185 146 5.9067 0.0185 147 5.9251 0.0184 148 5.9434 0.0183 149 5.9617 0.0183 150 5.9799 0.0182 151 5.9980 0.0181 152 6.0161 0.0181 153 6.0341 0.0180 154 6.0520 0.0179 155 6.0699 0.0179 156 6.0877 0.0178 157 6.1055 0.0178 158 6.1232 0.0177 159 6.1408 0.0176 160 6.1584 0.0176 161 6.1759 0.0175 162 6.1933 0.0175 163 6.2107 0.0174 164 6.2280 0.0173 165 6.2453 0.0173 166 6.2625 0.0172 167 6.2797 0.0172 168 6.2968 0.0171 169 6.3139 0.0171 170 6.3309 0.0170 171 6.3478 0.0169 172 6.3647 0.0169 173 6.3815 0.0168 174 6.3983 0.0168 175 6.4150 0.0167 176 6.4317 0.0167 177 6.4484 0.0166 178 6.4649 0.0166 179 6.4815 0.0165 180 6.4979 0.0165 181 6.5144 0.0164 182 6.5307 0.0164 183 6.5471 0.0163 184 6.5633 0.0163 185 6.5796 0.0162 186 6.5958 0.0162 187 6.6119 0.0161 188 6.6280 0.0161 189 6.6440 0.0160 190 6.6600 0.0160 191 6.6760 0.0160 192 6.6919 0.0159 193 6.7077 0.0159 194 6.7235 0.0158 195 6.7393 0.0158 196 6.7550 0.0157 197 6.7707 0.0157 198 6.7864 0.0156 199 6.8020 0.0156 200 6.8175 0.0156 201 6.8330 0.0155 202 6.8485 0.0155 203 6.8639 0.0154 204 6.8793 0.0154 205 6.8947 0.0153 206 6.9100 0.0153 207 6.9252 0.0153 208 6.9405 0.0152 209 6.9557 0.0152 210 6.9708 0.0151 211 6.9859 0.0151 212 7.0010 0.0151 213 7.0160 0.0150 214 7.0310 0.0150 215 7.0459 0.0150 216 7.0609 0.0149 217 7.0757 0.0149 218 7.0906 0.0148 219 7.1054 0.0148 220 7.1202 0.0148 221 7.1349 0.0147 222 7.1496 0.0147 223 7.1642 0.0147 224 7.1789 0.0146 225 7.1934 0.0146 226 7.2080 0.0146 227 7.2225 0.0145 228 7.2370 0.0145 229 7.2514 0.0144 230 7.2659 0.0144 231 7.2802 0.0144 232 7.2946 0.0143 233 7.3089 0.0143 234 7.3232 0.0143 235 7.3374 0.0142 236 7.3516 0.0142 237 7.3658 0.0142 238 7.3799 0.0141 239 7.3941 0.0141 240 7.4081 0.0141 241 7.4222 0.0141 242 7.4362 0.0140 243 7.4502 0.0140 244 7.4642 0.0140 245 7.4781 0.0139 246 7.4920 0.0139 247 7.5058 0.0139 248 7.5197 0.0138 249 7.5335 0.0138 250 7.5472 0.0138 251 7.5610 0.0137 252 7.5747 0.0137 253 7.5884 0.0137 254 7.6020 0.0137 255 7.6157 0.0136 256 7.6293 0.0136 257 7.6428 0.0136 258 7.6564 0.0135 259 7.6699 0.0135 260 7.6833 0.0135 261 7.6968 0.0135 262 7.7102 0.0134 263 7.7236 0.0134 264 7.7370 0.0134 265 7.7503 0.0133 266 7.7636 0.0133 267 7.7769 0.0133 268 7.7902 0.0133 269 7.8034 0.0132 270 7.8166 0.0132 271 7.8298 0.0132 272 7.8430 0.0132 273 7.8561 0.0131 274 7.8692 0.0131 275 7.8823 0.0131 276 7.8953 0.0130 277 7.9083 0.0130 278 7.9213 0.0130 279 7.9343 0.0130 280 7.9473 0.0129 281 7.9602 0.0129 282 7.9731 0.0129 283 7.9859 0.0129 284 7.9988 0.0128 285 8.0116 0.0128 286 8.0244 0.0128 287 8.0372 0.0128 288 8.0499 0.0127 ‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐ Unit Unit Unit Effective Period Rainfall Soil‐Loss Rainfall (number) (In) (In) (In) ‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐ 1 0.0127 0.0056 0.0071 2 0.0128 0.0056 0.0072 3 0.0128 0.0056 0.0072 4 0.0128 0.0057 0.0072 5 0.0129 0.0057 0.0072 6 0.0129 0.0057 0.0072 7 0.0130 0.0057 0.0073 8 0.0130 0.0057 0.0073 9 0.0130 0.0057 0.0073 10 0.0131 0.0058 0.0073 11 0.0131 0.0058 0.0073 12 0.0132 0.0058 0.0074 13 0.0132 0.0058 0.0074 14 0.0132 0.0058 0.0074 15 0.0133 0.0058 0.0074 16 0.0133 0.0059 0.0075 17 0.0134 0.0059 0.0075 18 0.0134 0.0059 0.0075 19 0.0135 0.0059 0.0075 20 0.0135 0.0059 0.0075 21 0.0135 0.0060 0.0076 22 0.0136 0.0060 0.0076 23 0.0136 0.0060 0.0076 24 0.0137 0.0060 0.0076 25 0.0137 0.0060 0.0077 26 0.0137 0.0060 0.0077 27 0.0138 0.0061 0.0077 28 0.0138 0.0061 0.0077 29 0.0139 0.0061 0.0078 30 0.0139 0.0061 0.0078 31 0.0140 0.0062 0.0078 32 0.0140 0.0062 0.0078 33 0.0141 0.0062 0.0079 34 0.0141 0.0062 0.0079 35 0.0142 0.0062 0.0079 36 0.0142 0.0063 0.0080 37 0.0143 0.0063 0.0080 38 0.0143 0.0063 0.0080 39 0.0144 0.0063 0.0081 40 0.0144 0.0063 0.0081 41 0.0145 0.0064 0.0081 42 0.0145 0.0064 0.0081 43 0.0146 0.0064 0.0082 44 0.0146 0.0064 0.0082 45 0.0147 0.0065 0.0082 46 0.0147 0.0065 0.0082 47 0.0148 0.0065 0.0083 48 0.0148 0.0065 0.0083 49 0.0149 0.0066 0.0084 50 0.0150 0.0066 0.0084 51 0.0150 0.0066 0.0084 52 0.0151 0.0066 0.0084 53 0.0151 0.0067 0.0085 54 0.0152 0.0067 0.0085 55 0.0153 0.0067 0.0085 56 0.0153 0.0067 0.0086 57 0.0154 0.0068 0.0086 58 0.0154 0.0068 0.0086 59 0.0155 0.0068 0.0087 60 0.0156 0.0068 0.0087 61 0.0156 0.0069 0.0088 62 0.0157 0.0069 0.0088 63 0.0158 0.0069 0.0088 64 0.0158 0.0070 0.0089 65 0.0159 0.0070 0.0089 66 0.0160 0.0070 0.0089 67 0.0160 0.0071 0.0090 68 0.0161 0.0071 0.0090 69 0.0162 0.0071 0.0091 70 0.0162 0.0071 0.0091 71 0.0163 0.0072 0.0091 72 0.0164 0.0072 0.0092 73 0.0165 0.0073 0.0092 74 0.0165 0.0073 0.0093 75 0.0166 0.0073 0.0093 76 0.0167 0.0073 0.0093 77 0.0168 0.0074 0.0094 78 0.0168 0.0074 0.0094 79 0.0169 0.0075 0.0095 80 0.0170 0.0075 0.0095 81 0.0171 0.0075 0.0096 82 0.0172 0.0076 0.0096 83 0.0173 0.0076 0.0097 84 0.0173 0.0076 0.0097 85 0.0175 0.0077 0.0098 86 0.0175 0.0077 0.0098 87 0.0176 0.0078 0.0099 88 0.0177 0.0078 0.0099 89 0.0178 0.0078 0.0100 90 0.0179 0.0079 0.0100 91 0.0180 0.0079 0.0101 92 0.0181 0.0080 0.0101 93 0.0182 0.0080 0.0102 94 0.0183 0.0080 0.0102 95 0.0184 0.0081 0.0103 96 0.0185 0.0081 0.0103 97 0.0186 0.0082 0.0104 98 0.0187 0.0082 0.0105 99 0.0188 0.0083 0.0105 100 0.0189 0.0083 0.0106 101 0.0190 0.0084 0.0107 102 0.0191 0.0084 0.0107 103 0.0193 0.0085 0.0108 104 0.0194 0.0085 0.0108 105 0.0195 0.0086 0.0109 106 0.0196 0.0086 0.0110 107 0.0198 0.0087 0.0111 108 0.0198 0.0087 0.0111 109 0.0200 0.0088 0.0112 110 0.0201 0.0088 0.0113 111 0.0203 0.0089 0.0114 112 0.0204 0.0090 0.0114 113 0.0206 0.0090 0.0115 114 0.0207 0.0091 0.0116 115 0.0208 0.0092 0.0117 116 0.0209 0.0092 0.0117 117 0.0211 0.0093 0.0118 118 0.0212 0.0094 0.0119 119 0.0215 0.0094 0.0120 120 0.0216 0.0095 0.0121 121 0.0218 0.0096 0.0122 122 0.0219 0.0096 0.0123 123 0.0221 0.0097 0.0124 124 0.0222 0.0098 0.0124 125 0.0225 0.0099 0.0126 126 0.0226 0.0099 0.0126 127 0.0228 0.0101 0.0128 128 0.0230 0.0101 0.0129 129 0.0232 0.0102 0.0130 130 0.0234 0.0103 0.0131 131 0.0236 0.0104 0.0132 132 0.0238 0.0105 0.0133 133 0.0241 0.0106 0.0135 134 0.0242 0.0107 0.0136 135 0.0245 0.0108 0.0137 136 0.0247 0.0109 0.0138 137 0.0250 0.0110 0.0140 138 0.0252 0.0111 0.0141 139 0.0255 0.0112 0.0143 140 0.0257 0.0113 0.0144 141 0.0260 0.0115 0.0146 142 0.0262 0.0115 0.0147 143 0.0266 0.0117 0.0149 144 0.0268 0.0118 0.0150 145 0.0317 0.0140 0.0178 146 0.0319 0.0141 0.0179 147 0.0324 0.0142 0.0181 148 0.0326 0.0143 0.0182 149 0.0331 0.0145 0.0185 150 0.0333 0.0147 0.0186 151 0.0338 0.0149 0.0189 152 0.0340 0.0150 0.0191 153 0.0346 0.0152 0.0194 154 0.0349 0.0153 0.0195 155 0.0354 0.0156 0.0198 156 0.0357 0.0157 0.0200 157 0.0363 0.0160 0.0203 158 0.0367 0.0161 0.0205 159 0.0373 0.0164 0.0209 160 0.0377 0.0166 0.0211 161 0.0384 0.0169 0.0215 162 0.0388 0.0171 0.0217 163 0.0396 0.0174 0.0222 164 0.0400 0.0176 0.0224 165 0.0409 0.0180 0.0229 166 0.0414 0.0182 0.0232 167 0.0424 0.0187 0.0237 168 0.0429 0.0189 0.0240 169 0.0440 0.0194 0.0247 170 0.0446 0.0196 0.0250 171 0.0459 0.0202 0.0257 172 0.0466 0.0205 0.0261 173 0.0480 0.0211 0.0269 174 0.0488 0.0215 0.0273 175 0.0505 0.0222 0.0283 176 0.0514 0.0226 0.0288 177 0.0534 0.0235 0.0299 178 0.0545 0.0240 0.0305 179 0.0570 0.0251 0.0319 180 0.0583 0.0257 0.0326 181 0.0613 0.0270 0.0343 182 0.0630 0.0277 0.0353 183 0.0670 0.0295 0.0375 184 0.0692 0.0305 0.0388 185 0.0564 0.0248 0.0316 186 0.0596 0.0262 0.0334 187 0.0677 0.0298 0.0379 188 0.0729 0.0321 0.0408 189 0.0879 0.0387 0.0492 190 0.0992 0.0437 0.0556 191 0.1418 0.0444 0.0975 192 0.1951 0.0444 0.1507 193 0.6105 0.0444 0.5661 194 0.1155 0.0444 0.0712 195 0.0795 0.0350 0.0445 196 0.0633 0.0279 0.0354 197 0.0718 0.0316 0.0402 198 0.0649 0.0286 0.0363 199 0.0598 0.0263 0.0335 200 0.0557 0.0245 0.0312 201 0.0524 0.0231 0.0293 202 0.0496 0.0218 0.0278 203 0.0473 0.0208 0.0265 204 0.0453 0.0199 0.0253 205 0.0435 0.0191 0.0243 206 0.0419 0.0184 0.0235 207 0.0405 0.0178 0.0227 208 0.0392 0.0173 0.0219 209 0.0380 0.0167 0.0213 210 0.0370 0.0163 0.0207 211 0.0360 0.0159 0.0202 212 0.0351 0.0155 0.0197 213 0.0343 0.0151 0.0192 214 0.0335 0.0148 0.0188 215 0.0328 0.0144 0.0184 216 0.0322 0.0141 0.0180 217 0.0270 0.0119 0.0151 218 0.0264 0.0116 0.0148 219 0.0258 0.0114 0.0145 220 0.0253 0.0111 0.0142 221 0.0248 0.0109 0.0139 222 0.0244 0.0107 0.0136 223 0.0239 0.0105 0.0134 224 0.0235 0.0103 0.0132 225 0.0231 0.0102 0.0129 226 0.0227 0.0100 0.0127 227 0.0224 0.0098 0.0125 228 0.0220 0.0097 0.0123 229 0.0217 0.0095 0.0121 230 0.0213 0.0094 0.0120 231 0.0210 0.0093 0.0118 232 0.0207 0.0091 0.0116 233 0.0205 0.0090 0.0115 234 0.0202 0.0089 0.0113 235 0.0199 0.0088 0.0112 236 0.0197 0.0087 0.0110 237 0.0194 0.0086 0.0109 238 0.0192 0.0084 0.0108 239 0.0190 0.0083 0.0106 240 0.0188 0.0083 0.0105 241 0.0185 0.0082 0.0104 242 0.0183 0.0081 0.0103 243 0.0181 0.0080 0.0102 244 0.0179 0.0079 0.0100 245 0.0178 0.0078 0.0099 246 0.0176 0.0077 0.0098 247 0.0174 0.0077 0.0097 248 0.0172 0.0076 0.0096 249 0.0171 0.0075 0.0095 250 0.0169 0.0074 0.0095 251 0.0167 0.0074 0.0094 252 0.0166 0.0073 0.0093 253 0.0164 0.0072 0.0092 254 0.0163 0.0072 0.0091 255 0.0161 0.0071 0.0090 256 0.0160 0.0070 0.0090 257 0.0159 0.0070 0.0089 258 0.0157 0.0069 0.0088 259 0.0156 0.0069 0.0087 260 0.0155 0.0068 0.0087 261 0.0153 0.0068 0.0086 262 0.0152 0.0067 0.0085 263 0.0151 0.0066 0.0085 264 0.0150 0.0066 0.0084 265 0.0149 0.0065 0.0083 266 0.0148 0.0065 0.0083 267 0.0147 0.0065 0.0082 268 0.0146 0.0064 0.0081 269 0.0144 0.0064 0.0081 270 0.0143 0.0063 0.0080 271 0.0142 0.0063 0.0080 272 0.0141 0.0062 0.0079 273 0.0141 0.0062 0.0079 274 0.0140 0.0061 0.0078 275 0.0139 0.0061 0.0078 276 0.0138 0.0061 0.0077 277 0.0137 0.0060 0.0077 278 0.0136 0.0060 0.0076 279 0.0135 0.0059 0.0076 280 0.0134 0.0059 0.0075 281 0.0133 0.0059 0.0075 282 0.0133 0.0058 0.0074 283 0.0132 0.0058 0.0074 284 0.0131 0.0058 0.0073 285 0.0130 0.0057 0.0073 286 0.0129 0.0057 0.0072 287 0.0129 0.0057 0.0072 288 0.0128 0.0056 0.0072 ‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐ ‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐ Total soil rain loss = 3.25(In) Total effective rainfall = 4.80(In) Peak flow rate in flood hydrograph = 13.78(CFS) ‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐ ++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ 24 ‐ H O U R S T O R M R u n o f f H y d r o g r a p h ‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐ Hydrograph in 5 Minute intervals ((CFS)) ‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐ Time(h+m) Volume Ac.Ft Q(CFS) 0 5.0 10.0 15.0 20.0 ‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐ 0+ 5 0.0001 0.02 Q | | | | 0+10 0.0006 0.07 Q | | | | 0+15 0.0017 0.16 Q | | | | 0+20 0.0036 0.28 Q | | | | 0+25 0.0061 0.36 Q | | | | 0+30 0.0089 0.41 Q | | | | 0+35 0.0120 0.44 Q | | | | 0+40 0.0152 0.47 Q | | | | 0+45 0.0186 0.49 Q | | | | 0+50 0.0221 0.51 VQ | | | | 0+55 0.0257 0.52 VQ | | | | 1+ 0 0.0293 0.53 VQ | | | | 1+ 5 0.0331 0.54 VQ | | | | 1+10 0.0369 0.55 VQ | | | | 1+15 0.0408 0.56 VQ | | | | 1+20 0.0447 0.57 VQ | | | | 1+25 0.0487 0.58 VQ | | | | 1+30 0.0527 0.58 VQ | | | | 1+35 0.0567 0.59 VQ | | | | 1+40 0.0608 0.59 VQ | | | | 1+45 0.0649 0.60 VQ | | | | 1+50 0.0691 0.60 |Q | | | | 1+55 0.0733 0.61 |Q | | | | 2+ 0 0.0775 0.61 |Q | | | | 2+ 5 0.0818 0.62 |Q | | | | 2+10 0.0860 0.62 |Q | | | | 2+15 0.0903 0.62 |Q | | | | 2+20 0.0946 0.63 |Q | | | | 2+25 0.0990 0.63 |Q | | | | 2+30 0.1034 0.63 |Q | | | | 2+35 0.1077 0.64 |Q | | | | 2+40 0.1121 0.64 |Q | | | | 2+45 0.1165 0.64 |Q | | | | 2+50 0.1210 0.64 |Q | | | | 2+55 0.1254 0.64 |Q | | | | 3+ 0 0.1299 0.65 |Q | | | | 3+ 5 0.1343 0.65 |Q | | | | 3+10 0.1388 0.65 |QV | | | | 3+15 0.1433 0.65 |QV | | | | 3+20 0.1478 0.66 |QV | | | | 3+25 0.1524 0.66 |QV | | | | 3+30 0.1569 0.66 |QV | | | | 3+35 0.1615 0.66 |QV | | | | 3+40 0.1660 0.66 |QV | | | | 3+45 0.1706 0.67 |QV | | | | 3+50 0.1752 0.67 |QV | | | | 3+55 0.1799 0.67 |QV | | | | 4+ 0 0.1845 0.67 |QV | | | | 4+ 5 0.1892 0.68 |QV | | | | 4+10 0.1939 0.68 |QV | | | | 4+15 0.1986 0.68 |QV | | | | 4+20 0.2033 0.68 |QV | | | | 4+25 0.2080 0.69 |Q V | | | | 4+30 0.2127 0.69 |Q V | | | | 4+35 0.2175 0.69 |Q V | | | | 4+40 0.2223 0.69 |Q V | | | | 4+45 0.2271 0.70 |Q V | | | | 4+50 0.2319 0.70 |Q V | | | | 4+55 0.2368 0.70 |Q V | | | | 5+ 0 0.2416 0.71 |Q V | | | | 5+ 5 0.2465 0.71 |Q V | | | | 5+10 0.2514 0.71 |Q V | | | | 5+15 0.2563 0.71 |Q V | | | | 5+20 0.2613 0.72 |Q V | | | | 5+25 0.2662 0.72 |Q V | | | | 5+30 0.2712 0.72 |Q V | | | | 5+35 0.2762 0.73 |Q V | | | | 5+40 0.2812 0.73 |Q V | | | | 5+45 0.2862 0.73 |Q V | | | | 5+50 0.2913 0.74 |Q V | | | | 5+55 0.2964 0.74 |Q V | | | | 6+ 0 0.3015 0.74 |Q V | | | | 6+ 5 0.3066 0.74 |Q V | | | | 6+10 0.3118 0.75 |Q V | | | | 6+15 0.3170 0.75 |Q V | | | | 6+20 0.3222 0.75 |Q V | | | | 6+25 0.3274 0.76 |Q V | | | | 6+30 0.3326 0.76 |Q V | | | | 6+35 0.3379 0.76 |Q V | | | | 6+40 0.3432 0.77 |Q V | | | | 6+45 0.3485 0.77 |Q V | | | | 6+50 0.3538 0.78 |Q V | | | | 6+55 0.3592 0.78 |Q V | | | | 7+ 0 0.3646 0.78 |Q V | | | | 7+ 5 0.3700 0.79 |Q V | | | | 7+10 0.3755 0.79 |Q V | | | | 7+15 0.3809 0.79 |Q V | | | | 7+20 0.3864 0.80 |Q V | | | | 7+25 0.3919 0.80 |Q V | | | | 7+30 0.3975 0.81 |Q V | | | | 7+35 0.4031 0.81 |Q V | | | | 7+40 0.4087 0.81 |Q V | | | | 7+45 0.4143 0.82 |Q V | | | | 7+50 0.4200 0.82 |Q V | | | | 7+55 0.4257 0.83 |Q V | | | | 8+ 0 0.4314 0.83 |Q V | | | | 8+ 5 0.4372 0.84 |Q V | | | | 8+10 0.4430 0.84 |Q V | | | | 8+15 0.4488 0.85 |Q V | | | | 8+20 0.4546 0.85 |Q V | | | | 8+25 0.4605 0.85 |Q V | | | | 8+30 0.4665 0.86 |Q V | | | | 8+35 0.4724 0.86 |Q V | | | | 8+40 0.4784 0.87 |Q V | | | | 8+45 0.4844 0.87 |Q V | | | | 8+50 0.4905 0.88 |Q V | | | | 8+55 0.4966 0.89 |Q V | | | | 9+ 0 0.5027 0.89 |Q V | | | | 9+ 5 0.5089 0.90 |Q V | | | | 9+10 0.5151 0.90 |Q V | | | | 9+15 0.5213 0.91 |Q V | | | | 9+20 0.5276 0.91 |Q V | | | | 9+25 0.5340 0.92 |Q V | | | | 9+30 0.5403 0.92 |Q V | | | | 9+35 0.5467 0.93 |Q V | | | | 9+40 0.5532 0.94 |Q V | | | | 9+45 0.5597 0.94 |Q V | | | | 9+50 0.5662 0.95 |Q V | | | | 9+55 0.5728 0.96 |Q V | | | | 10+ 0 0.5794 0.96 |Q V | | | | 10+ 5 0.5861 0.97 |Q V | | | | 10+10 0.5928 0.98 |Q V | | | | 10+15 0.5996 0.98 |Q V | | | | 10+20 0.6064 0.99 |Q V | | | | 10+25 0.6133 1.00 |Q V | | | | 10+30 0.6202 1.01 | Q V| | | | 10+35 0.6272 1.01 | Q V| | | | 10+40 0.6342 1.02 | Q V| | | | 10+45 0.6413 1.03 | Q V| | | | 10+50 0.6485 1.04 | Q V| | | | 10+55 0.6557 1.05 | Q V| | | | 11+ 0 0.6629 1.05 | Q V| | | | 11+ 5 0.6703 1.06 | Q V| | | | 11+10 0.6776 1.07 | Q V| | | | 11+15 0.6851 1.08 | Q V | | | 11+20 0.6926 1.09 | Q V | | | 11+25 0.7002 1.10 | Q V | | | 11+30 0.7078 1.11 | Q V | | | 11+35 0.7156 1.12 | Q V | | | 11+40 0.7234 1.13 | Q V | | | 11+45 0.7312 1.14 | Q V | | | 11+50 0.7392 1.15 | Q V | | | 11+55 0.7472 1.17 | Q V | | | 12+ 0 0.7553 1.18 | Q |V | | | 12+ 5 0.7635 1.19 | Q |V | | | 12+10 0.7720 1.23 | Q |V | | | 12+15 0.7807 1.27 | Q |V | | | 12+20 0.7899 1.33 | Q |V | | | 12+25 0.7993 1.37 | Q |V | | | 12+30 0.8089 1.40 | Q |V | | | 12+35 0.8188 1.43 | Q |V | | | 12+40 0.8288 1.45 | Q | V | | | 12+45 0.8389 1.47 | Q | V | | | 12+50 0.8492 1.49 | Q | V | | | 12+55 0.8596 1.52 | Q | V | | | 13+ 0 0.8702 1.54 | Q | V | | | 13+ 5 0.8809 1.56 | Q | V | | | 13+10 0.8918 1.58 | Q | V | | | 13+15 0.9028 1.60 | Q | V | | | 13+20 0.9140 1.62 | Q | V | | | 13+25 0.9253 1.65 | Q | V | | | 13+30 0.9368 1.67 | Q | V | | | 13+35 0.9485 1.69 | Q | V | | | 13+40 0.9603 1.72 | Q | V | | | 13+45 0.9723 1.74 | Q | V | | | 13+50 0.9845 1.77 | Q | V | | | 13+55 0.9969 1.80 | Q | V | | | 14+ 0 1.0095 1.83 | Q | V | | | 14+ 5 1.0223 1.86 | Q | V | | | 14+10 1.0353 1.89 | Q | V | | | 14+15 1.0485 1.92 | Q | V | | | 14+20 1.0620 1.96 | Q | V | | | 14+25 1.0758 2.00 | Q | V | | | 14+30 1.0898 2.04 | Q | V | | | 14+35 1.1042 2.08 | Q | V | | | 14+40 1.1188 2.13 | Q | V | | | 14+45 1.1338 2.18 | Q | V | | | 14+50 1.1491 2.23 | Q | V | | | 14+55 1.1649 2.29 | Q | V | | | 15+ 0 1.1810 2.35 | Q | V | | | 15+ 5 1.1977 2.41 | Q | V | | | 15+10 1.2148 2.49 | Q | V | | | 15+15 1.2325 2.57 | Q | V | | | 15+20 1.2509 2.66 | Q | V | | | 15+25 1.2698 2.75 | Q | V | | | 15+30 1.2890 2.79 | Q | V | | | 15+35 1.3083 2.79 | Q | V| | | 15+40 1.3275 2.80 | Q | V| | | 15+45 1.3474 2.88 | Q | V| | | 15+50 1.3685 3.06 | Q | V | | 15+55 1.3920 3.42 | Q | V | | 16+ 0 1.4204 4.13 | Q | V | | 16+ 5 1.4632 6.21 | | Q |V | | 16+10 1.5306 9.79 | | Q| V | | 16+15 1.6200 12.99 | | | V Q | | 16+20 1.7149 13.78 | | | V Q | | 16+25 1.7910 11.05 | | | Q V | | 16+30 1.8461 8.01 | | Q | V | | 16+35 1.8892 6.26 | | Q | V | | 16+40 1.9265 5.41 | Q | V | | 16+45 1.9601 4.87 | Q| | V | | 16+50 1.9907 4.44 | Q | | V| | 16+55 2.0187 4.07 | Q | | V| | 17+ 0 2.0443 3.72 | Q | | V| | 17+ 5 2.0684 3.50 | Q | | V | 17+10 2.0907 3.23 | Q | | V | 17+15 2.1116 3.04 | Q | | V | 17+20 2.1311 2.83 | Q | | |V | 17+25 2.1498 2.71 | Q | | |V | 17+30 2.1677 2.60 | Q | | |V | 17+35 2.1848 2.48 | Q | | |V | 17+40 2.2010 2.34 | Q | | | V | 17+45 2.2164 2.25 | Q | | | V | 17+50 2.2313 2.15 | Q | | | V | 17+55 2.2455 2.06 | Q | | | V | 18+ 0 2.2591 1.98 | Q | | | V | 18+ 5 2.2722 1.89 | Q | | | V | 18+10 2.2847 1.82 | Q | | | V | 18+15 2.2967 1.74 | Q | | | V | 18+20 2.3080 1.65 | Q | | | V | 18+25 2.3189 1.57 | Q | | | V | 18+30 2.3289 1.46 | Q | | | V | 18+35 2.3381 1.34 | Q | | | V | 18+40 2.3470 1.29 | Q | | | V | 18+45 2.3557 1.26 | Q | | | V | 18+50 2.3641 1.22 | Q | | | V | 18+55 2.3724 1.19 | Q | | | V | 19+ 0 2.3804 1.17 | Q | | | V | 19+ 5 2.3882 1.14 | Q | | | V | 19+10 2.3959 1.12 | Q | | | V | 19+15 2.4035 1.09 | Q | | | V | 19+20 2.4109 1.07 | Q | | | V | 19+25 2.4181 1.05 | Q | | | V | 19+30 2.4252 1.03 | Q | | | V | 19+35 2.4322 1.02 | Q | | | V | 19+40 2.4391 1.00 |Q | | | V | 19+45 2.4459 0.98 |Q | | | V | 19+50 2.4526 0.97 |Q | | | V | 19+55 2.4591 0.95 |Q | | | V | 20+ 0 2.4656 0.94 |Q | | | V | 20+ 5 2.4720 0.93 |Q | | | V | 20+10 2.4783 0.91 |Q | | | V | 20+15 2.4845 0.90 |Q | | | V | 20+20 2.4907 0.89 |Q | | | V | 20+25 2.4967 0.88 |Q | | | V | 20+30 2.5027 0.87 |Q | | | V | 20+35 2.5086 0.86 |Q | | | V | 20+40 2.5145 0.85 |Q | | | V | 20+45 2.5203 0.84 |Q | | | V | 20+50 2.5260 0.83 |Q | | | V | 20+55 2.5316 0.82 |Q | | | V | 21+ 0 2.5372 0.81 |Q | | | V | 21+ 5 2.5428 0.81 |Q | | | V | 21+10 2.5483 0.80 |Q | | | V | 21+15 2.5537 0.79 |Q | | | V | 21+20 2.5591 0.78 |Q | | | V | 21+25 2.5644 0.77 |Q | | | V | 21+30 2.5697 0.77 |Q | | | V | 21+35 2.5750 0.76 |Q | | | V | 21+40 2.5801 0.75 |Q | | | V | 21+45 2.5853 0.75 |Q | | | V | 21+50 2.5904 0.74 |Q | | | V | 21+55 2.5954 0.73 |Q | | | V | 22+ 0 2.6004 0.73 |Q | | | V | 22+ 5 2.6054 0.72 |Q | | | V | 22+10 2.6103 0.72 |Q | | | V | 22+15 2.6152 0.71 |Q | | | V | 22+20 2.6201 0.70 |Q | | | V | 22+25 2.6249 0.70 |Q | | | V | 22+30 2.6297 0.69 |Q | | | V | 22+35 2.6344 0.69 |Q | | | V | 22+40 2.6391 0.68 |Q | | | V | 22+45 2.6438 0.68 |Q | | | V | 22+50 2.6484 0.67 |Q | | | V | 22+55 2.6530 0.67 |Q | | | V | 23+ 0 2.6576 0.66 |Q | | | V | 23+ 5 2.6621 0.66 |Q | | | V | 23+10 2.6666 0.65 |Q | | | V| 23+15 2.6711 0.65 |Q | | | V| 23+20 2.6756 0.65 |Q | | | V| 23+25 2.6800 0.64 |Q | | | V| 23+30 2.6844 0.64 |Q | | | V| 23+35 2.6887 0.63 |Q | | | V| 23+40 2.6930 0.63 |Q | | | V| 23+45 2.6973 0.62 |Q | | | V| 23+50 2.7016 0.62 |Q | | | V| 23+55 2.7059 0.62 |Q | | | V| 24+ 0 2.7101 0.61 |Q | | | V| 24+ 5 2.7142 0.59 |Q | | | V| 24+10 2.7179 0.54 |Q | | | V| 24+15 2.7209 0.44 Q | | | V| 24+20 2.7232 0.32 Q | | | V| 24+25 2.7248 0.24 Q | | | V| 24+30 2.7261 0.19 Q | | | V| 24+35 2.7272 0.16 Q | | | V| 24+40 2.7281 0.13 Q | | | V| 24+45 2.7288 0.11 Q | | | V| 24+50 2.7295 0.10 Q | | | V| 24+55 2.7301 0.08 Q | | | V| 25+ 0 2.7305 0.07 Q | | | V| 25+ 5 2.7310 0.06 Q | | | V| 25+10 2.7313 0.05 Q | | | V| 25+15 2.7316 0.05 Q | | | V| 25+20 2.7319 0.04 Q | | | V| 25+25 2.7321 0.03 Q | | | V| 25+30 2.7323 0.03 Q | | | V| 25+35 2.7325 0.02 Q | | | V| 25+40 2.7327 0.02 Q | | | V| 25+45 2.7328 0.02 Q | | | V| 25+50 2.7329 0.01 Q | | | V| 25+55 2.7330 0.01 Q | | | V| 26+ 0 2.7330 0.01 Q | | | V| 26+ 5 2.7331 0.01 Q | | | V| 26+10 2.7331 0.01 Q | | | V| 26+15 2.7332 0.00 Q | | | V| 26+20 2.7332 0.00 Q | | | V| 26+25 2.7332 0.00 Q | | | V| ‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐ PROPOSED CONDITION U n i t H y d r o g r a p h A n a l y s i s Copyright (c) CIVILCADD/CIVILDESIGN, 1989 ‐ 2018, Version 9.0 Study date 12/01/22 ++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ ‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐ San Bernardino County Synthetic Unit Hydrology Method Manual date ‐ August 1986 Program License Serial Number 6427 ‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐ ‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐ Storm Event Year = 100 Antecedent Moisture Condition = 2 English (in‐lb) Input Units Used English Rainfall Data (Inches) Input Values Used English Units used in output format Area averaged rainfall intensity isohyetal data: Sub‐Area Duration Isohyetal (Ac.) (hours) (In) Rainfall data for year 100 6.84 1 1.65 ‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐ Rainfall data for year 100 6.84 6 4.28 ‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐ Rainfall data for year 100 6.84 24 8.05 ‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐ ++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ ******** Area‐averaged max loss rate, Fm ******** SCS curve SCS curve Area Area Fp(Fig C6) Ap Fm No.(AMCII) NO.(AMC 2) (Ac.) Fraction (In/Hr) (dec.) (In/Hr) 32.0 32.0 6.84 1.000 0.978 0.350 0.342 Area‐averaged adjusted loss rate Fm (In/Hr) = 0.342 ********* Area‐Averaged low loss rate fraction, Yb ********** Area Area SCS CN SCS CN S Pervious (Ac.) Fract (AMC2) (AMC2) Yield Fr 2.39 0.350 32.0 32.0 21.25 0.072 4.45 0.650 98.0 98.0 0.20 0.970 Area‐averaged catchment yield fraction, Y = 0.656 Area‐averaged low loss fraction, Yb = 0.344 User entry of time of concentration = 0.144 (hours) ++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ Watershed area = 6.84(Ac.) Catchment Lag time = 0.115 hours Unit interval = 5.000 minutes Unit interval percentage of lag time = 72.3380 Hydrograph baseflow = 0.00(CFS) Average maximum watershed loss rate(Fm) = 0.342(In/Hr) Average low loss rate fraction (Yb) = 0.344 (decimal) VALLEY DEVELOPED S‐Graph Selected Computed peak 5‐minute rainfall = 0.611(In) Computed peak 30‐minute rainfall = 1.250(In) Specified peak 1‐hour rainfall = 1.650(In) Computed peak 3‐hour rainfall = 2.960(In) Specified peak 6‐hour rainfall = 4.280(In) Specified peak 24‐hour rainfall = 8.050(In) Rainfall depth area reduction factors: Using a total area of 6.84(Ac.) (Ref: fig. E‐4) 5‐minute factor = 1.000 Adjusted rainfall = 0.610(In) 30‐minute factor = 1.000 Adjusted rainfall = 1.250(In) 1‐hour factor = 1.000 Adjusted rainfall = 1.649(In) 3‐hour factor = 1.000 Adjusted rainfall = 2.960(In) 6‐hour factor = 1.000 Adjusted rainfall = 4.280(In) 24‐hour factor = 1.000 Adjusted rainfall = 8.050(In) ‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐ U n i t H y d r o g r a p h +++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ Interval 'S' Graph Unit Hydrograph Number Mean values ((CFS)) ‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐ (K = 82.72 (CFS)) 1 9.344 7.729 2 55.996 38.591 3 90.659 28.674 4 98.201 6.239 5 100.000 1.488 ‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐ Peak Unit Adjusted mass rainfall Unit rainfall Number (In) (In) 1 0.6105 0.6105 2 0.8055 0.1951 3 0.9474 0.1418 4 1.0629 0.1155 5 1.1621 0.0992 6 1.2501 0.0879 7 1.3296 0.0795 8 1.4025 0.0729 9 1.4702 0.0677 10 1.5335 0.0633 11 1.5930 0.0596 12 1.6495 0.0564 13 1.7213 0.0718 14 1.7905 0.0692 15 1.8575 0.0670 16 1.9224 0.0649 17 1.9854 0.0630 18 2.0468 0.0613 19 2.1065 0.0598 20 2.1648 0.0583 21 2.2218 0.0570 22 2.2775 0.0557 23 2.3320 0.0545 24 2.3854 0.0534 25 2.4378 0.0524 26 2.4892 0.0514 27 2.5397 0.0505 28 2.5894 0.0496 29 2.6382 0.0488 30 2.6862 0.0480 31 2.7335 0.0473 32 2.7801 0.0466 33 2.8260 0.0459 34 2.8713 0.0453 35 2.9159 0.0446 36 2.9600 0.0440 37 3.0034 0.0435 38 3.0463 0.0429 39 3.0887 0.0424 40 3.1306 0.0419 41 3.1720 0.0414 42 3.2129 0.0409 43 3.2534 0.0405 44 3.2934 0.0400 45 3.3330 0.0396 46 3.3722 0.0392 47 3.4111 0.0388 48 3.4495 0.0384 49 3.4875 0.0380 50 3.5252 0.0377 51 3.5625 0.0373 52 3.5995 0.0370 53 3.6362 0.0367 54 3.6725 0.0363 55 3.7086 0.0360 56 3.7443 0.0357 57 3.7797 0.0354 58 3.8148 0.0351 59 3.8497 0.0349 60 3.8843 0.0346 61 3.9186 0.0343 62 3.9526 0.0340 63 3.9864 0.0338 64 4.0200 0.0335 65 4.0532 0.0333 66 4.0863 0.0331 67 4.1191 0.0328 68 4.1517 0.0326 69 4.1841 0.0324 70 4.2162 0.0322 71 4.2482 0.0319 72 4.2799 0.0317 73 4.3069 0.0270 74 4.3337 0.0268 75 4.3603 0.0266 76 4.3867 0.0264 77 4.4129 0.0262 78 4.4389 0.0260 79 4.4647 0.0258 80 4.4904 0.0257 81 4.5159 0.0255 82 4.5412 0.0253 83 4.5664 0.0252 84 4.5914 0.0250 85 4.6162 0.0248 86 4.6409 0.0247 87 4.6654 0.0245 88 4.6897 0.0244 89 4.7139 0.0242 90 4.7380 0.0241 91 4.7619 0.0239 92 4.7857 0.0238 93 4.8093 0.0236 94 4.8328 0.0235 95 4.8562 0.0234 96 4.8794 0.0232 97 4.9025 0.0231 98 4.9255 0.0230 99 4.9483 0.0228 100 4.9710 0.0227 101 4.9936 0.0226 102 5.0161 0.0225 103 5.0385 0.0224 104 5.0607 0.0222 105 5.0828 0.0221 106 5.1048 0.0220 107 5.1267 0.0219 108 5.1485 0.0218 109 5.1701 0.0217 110 5.1917 0.0216 111 5.2132 0.0215 112 5.2345 0.0213 113 5.2558 0.0212 114 5.2769 0.0211 115 5.2979 0.0210 116 5.3189 0.0209 117 5.3397 0.0208 118 5.3605 0.0207 119 5.3811 0.0207 120 5.4017 0.0206 121 5.4222 0.0205 122 5.4425 0.0204 123 5.4628 0.0203 124 5.4830 0.0202 125 5.5031 0.0201 126 5.5231 0.0200 127 5.5431 0.0199 128 5.5629 0.0198 129 5.5827 0.0198 130 5.6024 0.0197 131 5.6220 0.0196 132 5.6415 0.0195 133 5.6609 0.0194 134 5.6803 0.0194 135 5.6996 0.0193 136 5.7188 0.0192 137 5.7379 0.0191 138 5.7569 0.0190 139 5.7759 0.0190 140 5.7948 0.0189 141 5.8136 0.0188 142 5.8324 0.0188 143 5.8511 0.0187 144 5.8697 0.0186 145 5.8882 0.0185 146 5.9067 0.0185 147 5.9251 0.0184 148 5.9434 0.0183 149 5.9617 0.0183 150 5.9799 0.0182 151 5.9980 0.0181 152 6.0161 0.0181 153 6.0341 0.0180 154 6.0520 0.0179 155 6.0699 0.0179 156 6.0877 0.0178 157 6.1055 0.0178 158 6.1232 0.0177 159 6.1408 0.0176 160 6.1584 0.0176 161 6.1759 0.0175 162 6.1933 0.0175 163 6.2107 0.0174 164 6.2280 0.0173 165 6.2453 0.0173 166 6.2625 0.0172 167 6.2797 0.0172 168 6.2968 0.0171 169 6.3139 0.0171 170 6.3309 0.0170 171 6.3478 0.0169 172 6.3647 0.0169 173 6.3815 0.0168 174 6.3983 0.0168 175 6.4150 0.0167 176 6.4317 0.0167 177 6.4484 0.0166 178 6.4649 0.0166 179 6.4815 0.0165 180 6.4979 0.0165 181 6.5144 0.0164 182 6.5307 0.0164 183 6.5471 0.0163 184 6.5633 0.0163 185 6.5796 0.0162 186 6.5958 0.0162 187 6.6119 0.0161 188 6.6280 0.0161 189 6.6440 0.0160 190 6.6600 0.0160 191 6.6760 0.0160 192 6.6919 0.0159 193 6.7077 0.0159 194 6.7235 0.0158 195 6.7393 0.0158 196 6.7550 0.0157 197 6.7707 0.0157 198 6.7864 0.0156 199 6.8020 0.0156 200 6.8175 0.0156 201 6.8330 0.0155 202 6.8485 0.0155 203 6.8639 0.0154 204 6.8793 0.0154 205 6.8947 0.0153 206 6.9100 0.0153 207 6.9252 0.0153 208 6.9405 0.0152 209 6.9557 0.0152 210 6.9708 0.0151 211 6.9859 0.0151 212 7.0010 0.0151 213 7.0160 0.0150 214 7.0310 0.0150 215 7.0459 0.0150 216 7.0609 0.0149 217 7.0757 0.0149 218 7.0906 0.0148 219 7.1054 0.0148 220 7.1202 0.0148 221 7.1349 0.0147 222 7.1496 0.0147 223 7.1642 0.0147 224 7.1789 0.0146 225 7.1934 0.0146 226 7.2080 0.0146 227 7.2225 0.0145 228 7.2370 0.0145 229 7.2514 0.0144 230 7.2659 0.0144 231 7.2802 0.0144 232 7.2946 0.0143 233 7.3089 0.0143 234 7.3232 0.0143 235 7.3374 0.0142 236 7.3516 0.0142 237 7.3658 0.0142 238 7.3799 0.0141 239 7.3941 0.0141 240 7.4081 0.0141 241 7.4222 0.0141 242 7.4362 0.0140 243 7.4502 0.0140 244 7.4642 0.0140 245 7.4781 0.0139 246 7.4920 0.0139 247 7.5058 0.0139 248 7.5197 0.0138 249 7.5335 0.0138 250 7.5472 0.0138 251 7.5610 0.0137 252 7.5747 0.0137 253 7.5884 0.0137 254 7.6020 0.0137 255 7.6157 0.0136 256 7.6293 0.0136 257 7.6428 0.0136 258 7.6564 0.0135 259 7.6699 0.0135 260 7.6833 0.0135 261 7.6968 0.0135 262 7.7102 0.0134 263 7.7236 0.0134 264 7.7370 0.0134 265 7.7503 0.0133 266 7.7636 0.0133 267 7.7769 0.0133 268 7.7902 0.0133 269 7.8034 0.0132 270 7.8166 0.0132 271 7.8298 0.0132 272 7.8430 0.0132 273 7.8561 0.0131 274 7.8692 0.0131 275 7.8823 0.0131 276 7.8953 0.0130 277 7.9083 0.0130 278 7.9213 0.0130 279 7.9343 0.0130 280 7.9473 0.0129 281 7.9602 0.0129 282 7.9731 0.0129 283 7.9859 0.0129 284 7.9988 0.0128 285 8.0116 0.0128 286 8.0244 0.0128 287 8.0372 0.0128 288 8.0499 0.0127 ‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐ Unit Unit Unit Effective Period Rainfall Soil‐Loss Rainfall (number) (In) (In) (In) ‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐ 1 0.0127 0.0044 0.0084 2 0.0128 0.0044 0.0084 3 0.0128 0.0044 0.0084 4 0.0128 0.0044 0.0084 5 0.0129 0.0044 0.0085 6 0.0129 0.0044 0.0085 7 0.0130 0.0045 0.0085 8 0.0130 0.0045 0.0085 9 0.0130 0.0045 0.0086 10 0.0131 0.0045 0.0086 11 0.0131 0.0045 0.0086 12 0.0132 0.0045 0.0086 13 0.0132 0.0045 0.0087 14 0.0132 0.0046 0.0087 15 0.0133 0.0046 0.0087 16 0.0133 0.0046 0.0087 17 0.0134 0.0046 0.0088 18 0.0134 0.0046 0.0088 19 0.0135 0.0046 0.0088 20 0.0135 0.0046 0.0088 21 0.0135 0.0047 0.0089 22 0.0136 0.0047 0.0089 23 0.0136 0.0047 0.0089 24 0.0137 0.0047 0.0090 25 0.0137 0.0047 0.0090 26 0.0137 0.0047 0.0090 27 0.0138 0.0048 0.0091 28 0.0138 0.0048 0.0091 29 0.0139 0.0048 0.0091 30 0.0139 0.0048 0.0091 31 0.0140 0.0048 0.0092 32 0.0140 0.0048 0.0092 33 0.0141 0.0048 0.0092 34 0.0141 0.0049 0.0093 35 0.0142 0.0049 0.0093 36 0.0142 0.0049 0.0093 37 0.0143 0.0049 0.0094 38 0.0143 0.0049 0.0094 39 0.0144 0.0050 0.0094 40 0.0144 0.0050 0.0095 41 0.0145 0.0050 0.0095 42 0.0145 0.0050 0.0095 43 0.0146 0.0050 0.0096 44 0.0146 0.0050 0.0096 45 0.0147 0.0051 0.0096 46 0.0147 0.0051 0.0097 47 0.0148 0.0051 0.0097 48 0.0148 0.0051 0.0097 49 0.0149 0.0051 0.0098 50 0.0150 0.0051 0.0098 51 0.0150 0.0052 0.0099 52 0.0151 0.0052 0.0099 53 0.0151 0.0052 0.0099 54 0.0152 0.0052 0.0100 55 0.0153 0.0053 0.0100 56 0.0153 0.0053 0.0100 57 0.0154 0.0053 0.0101 58 0.0154 0.0053 0.0101 59 0.0155 0.0053 0.0102 60 0.0156 0.0054 0.0102 61 0.0156 0.0054 0.0103 62 0.0157 0.0054 0.0103 63 0.0158 0.0054 0.0103 64 0.0158 0.0054 0.0104 65 0.0159 0.0055 0.0104 66 0.0160 0.0055 0.0105 67 0.0160 0.0055 0.0105 68 0.0161 0.0055 0.0105 69 0.0162 0.0056 0.0106 70 0.0162 0.0056 0.0106 71 0.0163 0.0056 0.0107 72 0.0164 0.0056 0.0107 73 0.0165 0.0057 0.0108 74 0.0165 0.0057 0.0108 75 0.0166 0.0057 0.0109 76 0.0167 0.0057 0.0109 77 0.0168 0.0058 0.0110 78 0.0168 0.0058 0.0110 79 0.0169 0.0058 0.0111 80 0.0170 0.0059 0.0111 81 0.0171 0.0059 0.0112 82 0.0172 0.0059 0.0113 83 0.0173 0.0059 0.0113 84 0.0173 0.0060 0.0114 85 0.0175 0.0060 0.0114 86 0.0175 0.0060 0.0115 87 0.0176 0.0061 0.0116 88 0.0177 0.0061 0.0116 89 0.0178 0.0061 0.0117 90 0.0179 0.0062 0.0117 91 0.0180 0.0062 0.0118 92 0.0181 0.0062 0.0118 93 0.0182 0.0063 0.0119 94 0.0183 0.0063 0.0120 95 0.0184 0.0063 0.0121 96 0.0185 0.0064 0.0121 97 0.0186 0.0064 0.0122 98 0.0187 0.0064 0.0122 99 0.0188 0.0065 0.0123 100 0.0189 0.0065 0.0124 101 0.0190 0.0066 0.0125 102 0.0191 0.0066 0.0125 103 0.0193 0.0066 0.0126 104 0.0194 0.0067 0.0127 105 0.0195 0.0067 0.0128 106 0.0196 0.0067 0.0128 107 0.0198 0.0068 0.0130 108 0.0198 0.0068 0.0130 109 0.0200 0.0069 0.0131 110 0.0201 0.0069 0.0132 111 0.0203 0.0070 0.0133 112 0.0204 0.0070 0.0134 113 0.0206 0.0071 0.0135 114 0.0207 0.0071 0.0135 115 0.0208 0.0072 0.0137 116 0.0209 0.0072 0.0137 117 0.0211 0.0073 0.0139 118 0.0212 0.0073 0.0139 119 0.0215 0.0074 0.0141 120 0.0216 0.0074 0.0141 121 0.0218 0.0075 0.0143 122 0.0219 0.0075 0.0144 123 0.0221 0.0076 0.0145 124 0.0222 0.0077 0.0146 125 0.0225 0.0077 0.0147 126 0.0226 0.0078 0.0148 127 0.0228 0.0079 0.0150 128 0.0230 0.0079 0.0151 129 0.0232 0.0080 0.0152 130 0.0234 0.0080 0.0153 131 0.0236 0.0081 0.0155 132 0.0238 0.0082 0.0156 133 0.0241 0.0083 0.0158 134 0.0242 0.0083 0.0159 135 0.0245 0.0084 0.0161 136 0.0247 0.0085 0.0162 137 0.0250 0.0086 0.0164 138 0.0252 0.0087 0.0165 139 0.0255 0.0088 0.0167 140 0.0257 0.0088 0.0168 141 0.0260 0.0090 0.0171 142 0.0262 0.0090 0.0172 143 0.0266 0.0092 0.0174 144 0.0268 0.0092 0.0176 145 0.0317 0.0109 0.0208 146 0.0319 0.0110 0.0209 147 0.0324 0.0111 0.0212 148 0.0326 0.0112 0.0214 149 0.0331 0.0114 0.0217 150 0.0333 0.0115 0.0218 151 0.0338 0.0116 0.0222 152 0.0340 0.0117 0.0223 153 0.0346 0.0119 0.0227 154 0.0349 0.0120 0.0229 155 0.0354 0.0122 0.0232 156 0.0357 0.0123 0.0234 157 0.0363 0.0125 0.0238 158 0.0367 0.0126 0.0240 159 0.0373 0.0129 0.0245 160 0.0377 0.0130 0.0247 161 0.0384 0.0132 0.0252 162 0.0388 0.0134 0.0254 163 0.0396 0.0136 0.0260 164 0.0400 0.0138 0.0263 165 0.0409 0.0141 0.0268 166 0.0414 0.0143 0.0271 167 0.0424 0.0146 0.0278 168 0.0429 0.0148 0.0281 169 0.0440 0.0152 0.0289 170 0.0446 0.0154 0.0293 171 0.0459 0.0158 0.0301 172 0.0466 0.0160 0.0305 173 0.0480 0.0165 0.0315 174 0.0488 0.0168 0.0320 175 0.0505 0.0174 0.0331 176 0.0514 0.0177 0.0337 177 0.0534 0.0184 0.0350 178 0.0545 0.0188 0.0358 179 0.0570 0.0196 0.0373 180 0.0583 0.0201 0.0382 181 0.0613 0.0211 0.0402 182 0.0630 0.0217 0.0413 183 0.0670 0.0231 0.0439 184 0.0692 0.0238 0.0454 185 0.0564 0.0194 0.0370 186 0.0596 0.0205 0.0391 187 0.0677 0.0233 0.0444 188 0.0729 0.0251 0.0478 189 0.0879 0.0285 0.0594 190 0.0992 0.0285 0.0707 191 0.1418 0.0285 0.1133 192 0.1951 0.0285 0.1665 193 0.6105 0.0285 0.5820 194 0.1155 0.0285 0.0870 195 0.0795 0.0274 0.0521 196 0.0633 0.0218 0.0415 197 0.0718 0.0247 0.0471 198 0.0649 0.0223 0.0426 199 0.0598 0.0206 0.0392 200 0.0557 0.0192 0.0365 201 0.0524 0.0180 0.0344 202 0.0496 0.0171 0.0325 203 0.0473 0.0163 0.0310 204 0.0453 0.0156 0.0297 205 0.0435 0.0150 0.0285 206 0.0419 0.0144 0.0275 207 0.0405 0.0139 0.0265 208 0.0392 0.0135 0.0257 209 0.0380 0.0131 0.0249 210 0.0370 0.0127 0.0243 211 0.0360 0.0124 0.0236 212 0.0351 0.0121 0.0230 213 0.0343 0.0118 0.0225 214 0.0335 0.0115 0.0220 215 0.0328 0.0113 0.0215 216 0.0322 0.0111 0.0211 217 0.0270 0.0093 0.0177 218 0.0264 0.0091 0.0173 219 0.0258 0.0089 0.0169 220 0.0253 0.0087 0.0166 221 0.0248 0.0085 0.0163 222 0.0244 0.0084 0.0160 223 0.0239 0.0082 0.0157 224 0.0235 0.0081 0.0154 225 0.0231 0.0080 0.0151 226 0.0227 0.0078 0.0149 227 0.0224 0.0077 0.0147 228 0.0220 0.0076 0.0144 229 0.0217 0.0075 0.0142 230 0.0213 0.0074 0.0140 231 0.0210 0.0072 0.0138 232 0.0207 0.0071 0.0136 233 0.0205 0.0070 0.0134 234 0.0202 0.0070 0.0132 235 0.0199 0.0069 0.0131 236 0.0197 0.0068 0.0129 237 0.0194 0.0067 0.0127 238 0.0192 0.0066 0.0126 239 0.0190 0.0065 0.0124 240 0.0188 0.0065 0.0123 241 0.0185 0.0064 0.0122 242 0.0183 0.0063 0.0120 243 0.0181 0.0062 0.0119 244 0.0179 0.0062 0.0118 245 0.0178 0.0061 0.0116 246 0.0176 0.0060 0.0115 247 0.0174 0.0060 0.0114 248 0.0172 0.0059 0.0113 249 0.0171 0.0059 0.0112 250 0.0169 0.0058 0.0111 251 0.0167 0.0058 0.0110 252 0.0166 0.0057 0.0109 253 0.0164 0.0057 0.0108 254 0.0163 0.0056 0.0107 255 0.0161 0.0056 0.0106 256 0.0160 0.0055 0.0105 257 0.0159 0.0055 0.0104 258 0.0157 0.0054 0.0103 259 0.0156 0.0054 0.0102 260 0.0155 0.0053 0.0101 261 0.0153 0.0053 0.0101 262 0.0152 0.0052 0.0100 263 0.0151 0.0052 0.0099 264 0.0150 0.0052 0.0098 265 0.0149 0.0051 0.0098 266 0.0148 0.0051 0.0097 267 0.0147 0.0050 0.0096 268 0.0146 0.0050 0.0095 269 0.0144 0.0050 0.0095 270 0.0143 0.0049 0.0094 271 0.0142 0.0049 0.0093 272 0.0141 0.0049 0.0093 273 0.0141 0.0048 0.0092 274 0.0140 0.0048 0.0092 275 0.0139 0.0048 0.0091 276 0.0138 0.0047 0.0090 277 0.0137 0.0047 0.0090 278 0.0136 0.0047 0.0089 279 0.0135 0.0047 0.0089 280 0.0134 0.0046 0.0088 281 0.0133 0.0046 0.0087 282 0.0133 0.0046 0.0087 283 0.0132 0.0045 0.0086 284 0.0131 0.0045 0.0086 285 0.0130 0.0045 0.0085 286 0.0129 0.0045 0.0085 287 0.0129 0.0044 0.0084 288 0.0128 0.0044 0.0084 ‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐ ‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐ Total soil rain loss = 2.51(In) Total effective rainfall = 5.54(In) Peak flow rate in flood hydrograph = 28.72(CFS) ‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐ ++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ 24 ‐ H O U R S T O R M R u n o f f H y d r o g r a p h ‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐ Hydrograph in 5 Minute intervals ((CFS)) ‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐ Time(h+m) Volume Ac.Ft Q(CFS) 0 7.5 15.0 22.5 30.0 ‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐ 0+ 5 0.0004 0.06 Q | | | | 0+10 0.0031 0.39 Q | | | | 0+15 0.0074 0.63 Q | | | | 0+20 0.0121 0.68 Q | | | | 0+25 0.0169 0.70 Q | | | | 0+30 0.0217 0.70 Q | | | | 0+35 0.0266 0.70 Q | | | | 0+40 0.0314 0.70 Q | | | | 0+45 0.0362 0.70 Q | | | | 0+50 0.0411 0.71 Q | | | | 0+55 0.0460 0.71 Q | | | | 1+ 0 0.0509 0.71 Q | | | | 1+ 5 0.0558 0.71 Q | | | | 1+10 0.0607 0.71 Q | | | | 1+15 0.0657 0.72 Q | | | | 1+20 0.0706 0.72 Q | | | | 1+25 0.0756 0.72 Q | | | | 1+30 0.0806 0.72 QV | | | | 1+35 0.0856 0.73 QV | | | | 1+40 0.0906 0.73 QV | | | | 1+45 0.0956 0.73 QV | | | | 1+50 0.1007 0.73 QV | | | | 1+55 0.1057 0.74 QV | | | | 2+ 0 0.1108 0.74 QV | | | | 2+ 5 0.1159 0.74 QV | | | | 2+10 0.1210 0.74 QV | | | | 2+15 0.1261 0.74 QV | | | | 2+20 0.1313 0.75 QV | | | | 2+25 0.1364 0.75 QV | | | | 2+30 0.1416 0.75 |Q | | | | 2+35 0.1468 0.75 |Q | | | | 2+40 0.1520 0.76 |Q | | | | 2+45 0.1573 0.76 |Q | | | | 2+50 0.1625 0.76 |QV | | | | 2+55 0.1678 0.76 |QV | | | | 3+ 0 0.1731 0.77 |QV | | | | 3+ 5 0.1784 0.77 |QV | | | | 3+10 0.1837 0.77 |QV | | | | 3+15 0.1890 0.78 |QV | | | | 3+20 0.1944 0.78 |QV | | | | 3+25 0.1998 0.78 |QV | | | | 3+30 0.2052 0.78 |QV | | | | 3+35 0.2106 0.79 |QV | | | | 3+40 0.2160 0.79 |QV | | | | 3+45 0.2215 0.79 |QV | | | | 3+50 0.2270 0.80 |QV | | | | 3+55 0.2325 0.80 |QV | | | | 4+ 0 0.2380 0.80 |Q V | | | | 4+ 5 0.2435 0.80 |Q V | | | | 4+10 0.2491 0.81 |Q V | | | | 4+15 0.2546 0.81 |Q V | | | | 4+20 0.2603 0.81 |Q V | | | | 4+25 0.2659 0.82 |Q V | | | | 4+30 0.2715 0.82 |Q V | | | | 4+35 0.2772 0.82 |Q V | | | | 4+40 0.2829 0.83 |Q V | | | | 4+45 0.2886 0.83 |Q V | | | | 4+50 0.2943 0.83 |Q V | | | | 4+55 0.3001 0.84 |Q V | | | | 5+ 0 0.3059 0.84 |Q V | | | | 5+ 5 0.3117 0.84 |Q V | | | | 5+10 0.3175 0.85 |Q V | | | | 5+15 0.3233 0.85 |Q V | | | | 5+20 0.3292 0.85 |Q V | | | | 5+25 0.3351 0.86 |Q V | | | | 5+30 0.3410 0.86 |Q V | | | | 5+35 0.3470 0.86 |Q V | | | | 5+40 0.3530 0.87 |Q V | | | | 5+45 0.3590 0.87 |Q V | | | | 5+50 0.3650 0.88 |Q V | | | | 5+55 0.3711 0.88 |Q V | | | | 6+ 0 0.3771 0.88 |Q V | | | | 6+ 5 0.3832 0.89 |Q V | | | | 6+10 0.3894 0.89 |Q V | | | | 6+15 0.3955 0.90 |Q V | | | | 6+20 0.4017 0.90 |Q V | | | | 6+25 0.4080 0.90 |Q V | | | | 6+30 0.4142 0.91 |Q V | | | | 6+35 0.4205 0.91 |Q V | | | | 6+40 0.4268 0.92 |Q V | | | | 6+45 0.4331 0.92 |Q V | | | | 6+50 0.4395 0.93 |Q V | | | | 6+55 0.4459 0.93 |Q V | | | | 7+ 0 0.4524 0.93 |Q V | | | | 7+ 5 0.4588 0.94 |Q V | | | | 7+10 0.4653 0.94 |Q V | | | | 7+15 0.4719 0.95 |Q V | | | | 7+20 0.4784 0.95 |Q V | | | | 7+25 0.4850 0.96 |Q V | | | | 7+30 0.4916 0.96 |Q V | | | | 7+35 0.4983 0.97 |Q V | | | | 7+40 0.5050 0.97 |Q V | | | | 7+45 0.5118 0.98 |Q V | | | | 7+50 0.5185 0.98 |Q V | | | | 7+55 0.5253 0.99 |Q V | | | | 8+ 0 0.5322 0.99 |Q V | | | | 8+ 5 0.5391 1.00 |Q V | | | | 8+10 0.5460 1.01 |Q V | | | | 8+15 0.5530 1.01 |Q V | | | | 8+20 0.5600 1.02 |Q V | | | | 8+25 0.5670 1.02 |Q V | | | | 8+30 0.5741 1.03 |Q V | | | | 8+35 0.5813 1.04 |Q V | | | | 8+40 0.5884 1.04 |Q V | | | | 8+45 0.5957 1.05 |Q V | | | | 8+50 0.6029 1.05 |Q V | | | | 8+55 0.6102 1.06 |Q V | | | | 9+ 0 0.6176 1.07 |Q V | | | | 9+ 5 0.6250 1.07 |Q V | | | | 9+10 0.6324 1.08 |Q V | | | | 9+15 0.6399 1.09 |Q V | | | | 9+20 0.6475 1.10 |Q V | | | | 9+25 0.6551 1.10 |Q V | | | | 9+30 0.6627 1.11 |Q V | | | | 9+35 0.6704 1.12 |Q V | | | | 9+40 0.6782 1.13 |Q V | | | | 9+45 0.6860 1.13 |Q V | | | | 9+50 0.6938 1.14 |Q V | | | | 9+55 0.7018 1.15 |Q V | | | | 10+ 0 0.7097 1.16 |Q V | | | | 10+ 5 0.7178 1.17 |Q V| | | | 10+10 0.7259 1.18 |Q V| | | | 10+15 0.7340 1.18 |Q V| | | | 10+20 0.7423 1.19 |Q V| | | | 10+25 0.7505 1.20 |Q V| | | | 10+30 0.7589 1.21 |Q V| | | | 10+35 0.7673 1.22 |Q V| | | | 10+40 0.7758 1.23 |Q V| | | | 10+45 0.7844 1.24 |Q V| | | | 10+50 0.7930 1.25 |Q V | | | 10+55 0.8017 1.26 |Q V | | | 11+ 0 0.8105 1.28 |Q V | | | 11+ 5 0.8193 1.29 |Q V | | | 11+10 0.8283 1.30 |Q V | | | 11+15 0.8373 1.31 |Q V | | | 11+20 0.8464 1.32 |Q V | | | 11+25 0.8556 1.33 |Q V | | | 11+30 0.8649 1.35 |Q V | | | 11+35 0.8742 1.36 |Q |V | | | 11+40 0.8837 1.37 |Q |V | | | 11+45 0.8933 1.39 |Q |V | | | 11+50 0.9029 1.40 |Q |V | | | 11+55 0.9127 1.42 |Q |V | | | 12+ 0 0.9226 1.43 |Q |V | | | 12+ 5 0.9327 1.47 |Q |V | | | 12+10 0.9437 1.60 | Q |V | | | 12+15 0.9555 1.70 | Q | V | | | 12+20 0.9674 1.74 | Q | V | | | 12+25 0.9796 1.76 | Q | V | | | 12+30 0.9919 1.78 | Q | V | | | 12+35 1.0043 1.80 | Q | V | | | 12+40 1.0168 1.82 | Q | V | | | 12+45 1.0295 1.84 | Q | V | | | 12+50 1.0423 1.86 | Q | V | | | 12+55 1.0553 1.88 | Q | V | | | 13+ 0 1.0684 1.91 | Q | V | | | 13+ 5 1.0817 1.93 | Q | V | | | 13+10 1.0952 1.96 | Q | V | | | 13+15 1.1088 1.98 | Q | V | | | 13+20 1.1226 2.01 | Q | V | | | 13+25 1.1367 2.04 | Q | V | | | 13+30 1.1509 2.07 | Q | V | | | 13+35 1.1653 2.10 | Q | V | | | 13+40 1.1800 2.13 | Q | V | | | 13+45 1.1949 2.16 | Q | V | | | 13+50 1.2100 2.20 | Q | V | | | 13+55 1.2254 2.23 | Q | V | | | 14+ 0 1.2411 2.27 | Q | V | | | 14+ 5 1.2570 2.32 | Q | V | | | 14+10 1.2733 2.36 | Q | V | | | 14+15 1.2899 2.41 | Q | V | | | 14+20 1.3068 2.46 | Q | V | | | 14+25 1.3241 2.51 | Q | V | | | 14+30 1.3418 2.57 | Q | V | | | 14+35 1.3599 2.63 | Q | V | | | 14+40 1.3785 2.70 | Q | V | | | 14+45 1.3975 2.77 | Q | V | | | 14+50 1.4172 2.85 | Q | V | | | 14+55 1.4374 2.93 | Q | V | | | 15+ 0 1.4582 3.03 | Q | V | | | 15+ 5 1.4798 3.13 | Q | V | | | 15+10 1.5022 3.25 | Q | V| | | 15+15 1.5255 3.38 | Q | V| | | 15+20 1.5499 3.54 | Q | V| | | 15+25 1.5748 3.62 | Q | V| | | 15+30 1.5980 3.37 | Q | V | | 15+35 1.6204 3.26 | Q | V | | 15+40 1.6445 3.50 | Q | V | | 15+45 1.6712 3.88 | Q | |V | | 15+50 1.7025 4.55 | Q | |V | | 15+55 1.7416 5.67 | Q | | V | | 16+ 0 1.7976 8.13 | Q | V | | 16+ 5 1.8988 14.70 | | Q| V | | 16+10 2.0966 28.72 | | | V | Q | 16+15 2.2458 21.66 | | | Q | | 16+20 2.3057 8.71 | |Q | V| | 16+25 2.3393 4.87 | Q | | V| | 16+30 2.3654 3.79 | Q | | V| | 16+35 2.3904 3.63 | Q | | V | 16+40 2.4136 3.37 | Q | | V | 16+45 2.4352 3.13 | Q | | V | 16+50 2.4554 2.93 | Q | | |V | 16+55 2.4744 2.77 | Q | | |V | 17+ 0 2.4925 2.63 | Q | | |V | 17+ 5 2.5098 2.51 | Q | | |V | 17+10 2.5264 2.40 | Q | | | V | 17+15 2.5423 2.31 | Q | | | V | 17+20 2.5577 2.23 | Q | | | V | 17+25 2.5725 2.16 | Q | | | V | 17+30 2.5870 2.09 | Q | | | V | 17+35 2.6010 2.03 | Q | | | V | 17+40 2.6146 1.98 | Q | | | V | 17+45 2.6279 1.93 | Q | | | V | 17+50 2.6408 1.88 | Q | | | V | 17+55 2.6535 1.84 | Q | | | V | 18+ 0 2.6659 1.80 | Q | | | V | 18+ 5 2.6779 1.74 | Q | | | V | 18+10 2.6888 1.59 | Q | | | V | 18+15 2.6989 1.47 |Q | | | V | 18+20 2.7087 1.42 |Q | | | V | 18+25 2.7183 1.39 |Q | | | V | 18+30 2.7276 1.36 |Q | | | V | 18+35 2.7368 1.33 |Q | | | V | 18+40 2.7458 1.31 |Q | | | V | 18+45 2.7547 1.29 |Q | | | V | 18+50 2.7634 1.26 |Q | | | V | 18+55 2.7719 1.24 |Q | | | V | 19+ 0 2.7803 1.22 |Q | | | V | 19+ 5 2.7886 1.20 |Q | | | V | 19+10 2.7968 1.18 |Q | | | V | 19+15 2.8048 1.17 |Q | | | V | 19+20 2.8127 1.15 |Q | | | V | 19+25 2.8205 1.13 |Q | | | V | 19+30 2.8282 1.12 |Q | | | V | 19+35 2.8358 1.10 |Q | | | V | 19+40 2.8433 1.09 |Q | | | V | 19+45 2.8507 1.07 |Q | | | V | 19+50 2.8580 1.06 |Q | | | V | 19+55 2.8652 1.05 |Q | | | V | 20+ 0 2.8723 1.03 |Q | | | V | 20+ 5 2.8794 1.02 |Q | | | V | 20+10 2.8863 1.01 |Q | | | V | 20+15 2.8932 1.00 |Q | | | V | 20+20 2.9000 0.99 |Q | | | V | 20+25 2.9068 0.98 |Q | | | V | 20+30 2.9134 0.97 |Q | | | V | 20+35 2.9200 0.96 |Q | | | V | 20+40 2.9265 0.95 |Q | | | V | 20+45 2.9330 0.94 |Q | | | V | 20+50 2.9394 0.93 |Q | | | V | 20+55 2.9457 0.92 |Q | | | V | 21+ 0 2.9520 0.91 |Q | | | V | 21+ 5 2.9582 0.90 |Q | | | V | 21+10 2.9644 0.89 |Q | | | V | 21+15 2.9705 0.89 |Q | | | V | 21+20 2.9766 0.88 |Q | | | V | 21+25 2.9826 0.87 |Q | | | V | 21+30 2.9885 0.86 |Q | | | V | 21+35 2.9944 0.86 |Q | | | V | 21+40 3.0003 0.85 |Q | | | V | 21+45 3.0061 0.84 |Q | | | V | 21+50 3.0118 0.84 |Q | | | V | 21+55 3.0175 0.83 |Q | | | V | 22+ 0 3.0232 0.82 |Q | | | V | 22+ 5 3.0288 0.82 |Q | | | V | 22+10 3.0344 0.81 |Q | | | V | 22+15 3.0399 0.80 |Q | | | V | 22+20 3.0454 0.80 |Q | | | V | 22+25 3.0509 0.79 |Q | | | V | 22+30 3.0563 0.79 |Q | | | V | 22+35 3.0617 0.78 |Q | | | V | 22+40 3.0670 0.78 |Q | | | V | 22+45 3.0723 0.77 |Q | | | V | 22+50 3.0776 0.76 |Q | | | V| 22+55 3.0828 0.76 |Q | | | V| 23+ 0 3.0880 0.75 |Q | | | V| 23+ 5 3.0931 0.75 Q | | | V| 23+10 3.0983 0.74 Q | | | V| 23+15 3.1034 0.74 Q | | | V| 23+20 3.1084 0.73 Q | | | V| 23+25 3.1135 0.73 Q | | | V| 23+30 3.1185 0.73 Q | | | V| 23+35 3.1234 0.72 Q | | | V| 23+40 3.1284 0.72 Q | | | V| 23+45 3.1333 0.71 Q | | | V| 23+50 3.1381 0.71 Q | | | V| 23+55 3.1430 0.70 Q | | | V| 24+ 0 3.1478 0.70 Q | | | V| 24+ 5 3.1522 0.63 Q | | | V| 24+10 3.1543 0.31 Q | | | V| 24+15 3.1547 0.06 Q | | | V| 24+20 3.1548 0.01 Q | | | V ‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐ APPENDIX F HYDROGRAPH ROUTING CALCULATION FLOOD HYDROGRAPH ROUTING PROGRAM Copyright (c) CIVILCADD/CIVILDESIGN, 1989 ‐ 2018 Study date: 12/01/22 ‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐ Program License Serial Number 6427 ‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐ ********************* HYDROGRAPH INFORMATION ********************** From study/file name: 20580duh.rte ****************************HYDROGRAPH DATA**************************** Number of intervals = 292 Time interval = 5.0 (Min.) Maximum/Peak flow rate = 28.719 (CFS) Total volume = 3.155 (Ac.Ft) Status of hydrographs being held in storage Stream 1 Stream 2 Stream 3 Stream 4 Stream 5 Peak (CFS) 0.000 0.000 0.000 0.000 0.000 Vol (Ac.Ft) 0.000 0.000 0.000 0.000 0.000 *********************************************************************** ++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ Process from Point/Station 100.000 to Point/Station 110.000 **** RETARDING BASIN ROUTING **** ______________________________________________________________________ User entry of depth‐outflow‐storage data ‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐ Total number of inflow hydrograph intervals = 292 Hydrograph time unit = 5.000 (Min.) Initial depth in storage basin = 0.00(Ft.) ‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐ ‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐ Initial basin depth = 0.00 (Ft.) Initial basin storage = 0.00 (Ac.Ft) Initial basin outflow = 0.00 (CFS) ‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐ ‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐ Depth vs. Storage and Depth vs. Discharge data: Basin Depth Storage Outflow (S‐O*dt/2) (S+O*dt/2) (Ft.) (Ac.Ft) (CFS) (Ac.Ft) (Ac.Ft) ‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐ 0.000 0.000 0.000 0.000 0.000 0.500 0.003 0.001 0.003 0.003 1.000 0.008 4.810 ‐0.009 0.025 1.500 0.014 15.730 ‐0.040 0.068 2.000 0.021 20.070 ‐0.048 0.090 2.500 0.028 20.070 ‐0.041 0.097 3.000 0.035 20.070 ‐0.034 0.104 3.500 0.042 20.070 ‐0.027 0.111 4.000 0.049 20.070 ‐0.020 0.118 4.500 0.056 20.070 ‐0.013 0.125 5.000 0.063 20.070 ‐0.006 0.132 5.500 0.070 20.070 0.001 0.139 6.000 0.076 20.070 0.007 0.145 6.500 0.081 20.070 0.012 0.150 ‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐ Hydrograph Detention Basin Routing ‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐ Graph values: 'I'= unit inflow; 'O'=outflow at time shown ‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐ Time Inflow Outflow Storage Depth (Hours) (CFS) (CFS) (Ac.Ft) .0 7.2 14.36 21.54 28.72 (Ft.) 0.083 0.06 0.00 0.000 O | | | | 0.04 0.167 0.39 0.00 0.002 O | | | | 0.30 0.250 0.63 0.51 0.004 O | | | | 0.55 0.333 0.68 0.73 0.004 O | | | | 0.58 0.417 0.70 0.66 0.004 O | | | | 0.57 0.500 0.70 0.71 0.004 O | | | | 0.57 0.583 0.70 0.69 0.004 O | | | | 0.57 0.667 0.70 0.71 0.004 O | | | | 0.57 0.750 0.70 0.70 0.004 O | | | | 0.57 0.833 0.71 0.71 0.004 O | | | | 0.57 0.917 0.71 0.71 0.004 O | | | | 0.57 1.000 0.71 0.71 0.004 O | | | | 0.57 1.083 0.71 0.71 0.004 O | | | | 0.57 1.167 0.71 0.71 0.004 O | | | | 0.57 1.250 0.72 0.72 0.004 O | | | | 0.57 1.333 0.72 0.72 0.004 O | | | | 0.57 1.417 0.72 0.72 0.004 O | | | | 0.57 1.500 0.72 0.72 0.004 O | | | | 0.58 1.583 0.73 0.73 0.004 O | | | | 0.58 1.667 0.73 0.73 0.004 O | | | | 0.58 1.750 0.73 0.73 0.004 O | | | | 0.58 1.833 0.73 0.73 0.004 O | | | | 0.58 1.917 0.74 0.73 0.004 O | | | | 0.58 2.000 0.74 0.74 0.004 O | | | | 0.58 2.083 0.74 0.74 0.004 O | | | | 0.58 2.167 0.74 0.74 0.004 O | | | | 0.58 2.250 0.74 0.74 0.004 O | | | | 0.58 2.333 0.75 0.75 0.004 O | | | | 0.58 2.417 0.75 0.75 0.004 O | | | | 0.58 2.500 0.75 0.75 0.004 O | | | | 0.58 2.583 0.75 0.75 0.004 O | | | | 0.58 2.667 0.76 0.76 0.004 O | | | | 0.58 2.750 0.76 0.76 0.004 O | | | | 0.58 2.833 0.76 0.76 0.004 O | | | | 0.58 2.917 0.76 0.76 0.004 O | | | | 0.58 3.000 0.77 0.77 0.004 O | | | | 0.58 3.083 0.77 0.77 0.004 O | | | | 0.58 3.167 0.77 0.77 0.004 O | | | | 0.58 3.250 0.78 0.78 0.004 O | | | | 0.58 3.333 0.78 0.78 0.004 O | | | | 0.58 3.417 0.78 0.78 0.004 O | | | | 0.58 3.500 0.78 0.78 0.004 O | | | | 0.58 3.583 0.79 0.79 0.004 O | | | | 0.58 3.667 0.79 0.79 0.004 O | | | | 0.58 3.750 0.79 0.79 0.004 O | | | | 0.58 3.833 0.80 0.79 0.004 O | | | | 0.58 3.917 0.80 0.80 0.004 O | | | | 0.58 4.000 0.80 0.80 0.004 O | | | | 0.58 4.083 0.80 0.80 0.004 O | | | | 0.58 4.167 0.81 0.81 0.004 O | | | | 0.58 4.250 0.81 0.81 0.004 O | | | | 0.58 4.333 0.81 0.81 0.004 O | | | | 0.58 4.417 0.82 0.82 0.004 O | | | | 0.58 4.500 0.82 0.82 0.004 O | | | | 0.59 4.583 0.82 0.82 0.004 O | | | | 0.59 4.667 0.83 0.83 0.004 O | | | | 0.59 4.750 0.83 0.83 0.004 O | | | | 0.59 4.833 0.83 0.83 0.004 O | | | | 0.59 4.917 0.84 0.84 0.004 O | | | | 0.59 5.000 0.84 0.84 0.004 O | | | | 0.59 5.083 0.84 0.84 0.004 O | | | | 0.59 5.167 0.85 0.85 0.004 O | | | | 0.59 5.250 0.85 0.85 0.004 O | | | | 0.59 5.333 0.85 0.85 0.004 O | | | | 0.59 5.417 0.86 0.86 0.004 O | | | | 0.59 5.500 0.86 0.86 0.004 O | | | | 0.59 5.583 0.86 0.86 0.004 O | | | | 0.59 5.667 0.87 0.87 0.004 O | | | | 0.59 5.750 0.87 0.87 0.004 O | | | | 0.59 5.833 0.88 0.87 0.004 O | | | | 0.59 5.917 0.88 0.88 0.004 O | | | | 0.59 6.000 0.88 0.88 0.004 O | | | | 0.59 6.083 0.89 0.89 0.004 O | | | | 0.59 6.167 0.89 0.89 0.004 O | | | | 0.59 6.250 0.90 0.89 0.004 O | | | | 0.59 6.333 0.90 0.90 0.004 |O | | | | 0.59 6.417 0.90 0.90 0.004 |O | | | | 0.59 6.500 0.91 0.91 0.004 |O | | | | 0.59 6.583 0.91 0.91 0.004 |O | | | | 0.59 6.667 0.92 0.92 0.004 |O | | | | 0.60 6.750 0.92 0.92 0.004 |O | | | | 0.60 6.833 0.93 0.92 0.004 |O | | | | 0.60 6.917 0.93 0.93 0.004 |O | | | | 0.60 7.000 0.93 0.93 0.004 |O | | | | 0.60 7.083 0.94 0.94 0.004 |O | | | | 0.60 7.167 0.94 0.94 0.004 |O | | | | 0.60 7.250 0.95 0.95 0.004 |O | | | | 0.60 7.333 0.95 0.95 0.004 |O | | | | 0.60 7.417 0.96 0.96 0.004 |O | | | | 0.60 7.500 0.96 0.96 0.004 |O | | | | 0.60 7.583 0.97 0.97 0.004 |O | | | | 0.60 7.667 0.97 0.97 0.004 |O | | | | 0.60 7.750 0.98 0.98 0.004 |O | | | | 0.60 7.833 0.98 0.98 0.004 |O | | | | 0.60 7.917 0.99 0.99 0.004 |O | | | | 0.60 8.000 0.99 0.99 0.004 |O | | | | 0.60 8.083 1.00 1.00 0.004 |O | | | | 0.60 8.167 1.01 1.01 0.004 |O | | | | 0.60 8.250 1.01 1.01 0.004 |O | | | | 0.60 8.333 1.02 1.02 0.004 |O | | | | 0.61 8.417 1.02 1.02 0.004 |O | | | | 0.61 8.500 1.03 1.03 0.004 |O | | | | 0.61 8.583 1.04 1.03 0.004 |O | | | | 0.61 8.667 1.04 1.04 0.004 |O | | | | 0.61 8.750 1.05 1.05 0.004 |O | | | | 0.61 8.833 1.05 1.05 0.004 |O | | | | 0.61 8.917 1.06 1.06 0.004 |O | | | | 0.61 9.000 1.07 1.07 0.004 |O | | | | 0.61 9.083 1.07 1.07 0.004 |O | | | | 0.61 9.167 1.08 1.08 0.004 |O | | | | 0.61 9.250 1.09 1.09 0.004 |O | | | | 0.61 9.333 1.10 1.09 0.004 |O | | | | 0.61 9.417 1.10 1.10 0.004 |O | | | | 0.61 9.500 1.11 1.11 0.004 |O | | | | 0.62 9.583 1.12 1.12 0.004 |O | | | | 0.62 9.667 1.13 1.12 0.004 |O | | | | 0.62 9.750 1.13 1.13 0.004 |O | | | | 0.62 9.833 1.14 1.14 0.004 |O | | | | 0.62 9.917 1.15 1.15 0.004 |O | | | | 0.62 10.000 1.16 1.16 0.004 |O | | | | 0.62 10.083 1.17 1.17 0.004 |O | | | | 0.62 10.167 1.18 1.17 0.004 |O | | | | 0.62 10.250 1.18 1.18 0.004 |O | | | | 0.62 10.333 1.19 1.19 0.004 |O | | | | 0.62 10.417 1.20 1.20 0.004 |O | | | | 0.62 10.500 1.21 1.21 0.004 |O | | | | 0.63 10.583 1.22 1.22 0.004 |O | | | | 0.63 10.667 1.23 1.23 0.004 |O | | | | 0.63 10.750 1.24 1.24 0.004 |O | | | | 0.63 10.833 1.25 1.25 0.004 |O | | | | 0.63 10.917 1.26 1.26 0.004 |O | | | | 0.63 11.000 1.28 1.27 0.004 |O | | | | 0.63 11.083 1.29 1.28 0.004 |O | | | | 0.63 11.167 1.30 1.30 0.004 |O | | | | 0.63 11.250 1.31 1.31 0.004 |O | | | | 0.64 11.333 1.32 1.32 0.004 |O | | | | 0.64 11.417 1.33 1.33 0.004 |O | | | | 0.64 11.500 1.35 1.35 0.004 |O | | | | 0.64 11.583 1.36 1.36 0.004 |O | | | | 0.64 11.667 1.37 1.37 0.004 |O | | | | 0.64 11.750 1.39 1.39 0.004 |O | | | | 0.64 11.833 1.40 1.40 0.004 |O | | | | 0.65 11.917 1.42 1.42 0.004 |O | | | | 0.65 12.000 1.43 1.43 0.004 |O | | | | 0.65 12.083 1.47 1.46 0.005 |O | | | | 0.65 12.167 1.60 1.58 0.005 |O | | | | 0.66 12.250 1.70 1.69 0.005 |O | | | | 0.68 12.333 1.74 1.74 0.005 |O | | | | 0.68 12.417 1.76 1.76 0.005 |O | | | | 0.68 12.500 1.78 1.78 0.005 |O | | | | 0.68 12.583 1.80 1.80 0.005 | O | | | | 0.69 12.667 1.82 1.82 0.005 | O | | | | 0.69 12.750 1.84 1.84 0.005 | O | | | | 0.69 12.833 1.86 1.86 0.005 | O | | | | 0.69 12.917 1.88 1.88 0.005 | O | | | | 0.70 13.000 1.91 1.90 0.005 | O | | | | 0.70 13.083 1.93 1.93 0.005 | O | | | | 0.70 13.167 1.96 1.95 0.005 | O | | | | 0.70 13.250 1.98 1.98 0.005 | O | | | | 0.71 13.333 2.01 2.00 0.005 | O | | | | 0.71 13.417 2.04 2.03 0.005 | O | | | | 0.71 13.500 2.07 2.06 0.005 | O | | | | 0.71 13.583 2.10 2.09 0.005 | O | | | | 0.72 13.667 2.13 2.12 0.005 | O | | | | 0.72 13.750 2.16 2.16 0.005 | O | | | | 0.72 13.833 2.20 2.19 0.005 | O | | | | 0.73 13.917 2.23 2.23 0.005 | O | | | | 0.73 14.000 2.27 2.27 0.005 | O | | | | 0.74 14.083 2.32 2.31 0.005 | O | | | | 0.74 14.167 2.36 2.35 0.005 | O | | | | 0.74 14.250 2.41 2.40 0.005 | O | | | | 0.75 14.333 2.46 2.45 0.006 | O | | | | 0.75 14.417 2.51 2.50 0.006 | O | | | | 0.76 14.500 2.57 2.56 0.006 | O | | | | 0.77 14.583 2.63 2.62 0.006 | O | | | | 0.77 14.667 2.70 2.69 0.006 | OI | | | | 0.78 14.750 2.77 2.76 0.006 | O | | | | 0.79 14.833 2.85 2.84 0.006 | O | | | | 0.79 14.917 2.93 2.92 0.006 | O | | | | 0.80 15.000 3.03 3.01 0.006 | O | | | | 0.81 15.083 3.13 3.12 0.006 | O | | | | 0.82 15.167 3.25 3.23 0.006 | O | | | | 0.84 15.250 3.38 3.36 0.006 | O | | | | 0.85 15.333 3.54 3.51 0.007 | O | | | | 0.87 15.417 3.62 3.61 0.007 | O | | | | 0.88 15.500 3.37 3.43 0.007 | O | | | | 0.86 15.583 3.26 3.25 0.006 | O | | | | 0.84 15.667 3.50 3.45 0.007 | O | | | | 0.86 15.750 3.88 3.82 0.007 | O | | | | 0.90 15.833 4.55 4.42 0.008 | OI | | | | 0.96 15.917 5.67 5.56 0.008 | O | | | | 1.03 16.000 8.13 7.87 0.010 | OI | | | 1.14 16.083 14.70 13.98 0.013 | | OI | | 1.42 16.167 28.72 20.07 0.045 | | | O | I 3.74 16.250 21.66 20.07 0.081 | | | O I | 6.45 16.333 8.71 20.07 0.047 | |I | O | | 3.85 16.417 4.87 4.80 0.008 | O | | | | 1.00 16.500 3.79 4.08 0.007 | O | | | | 0.92 16.583 3.63 3.51 0.007 | OI | | | | 0.87 16.667 3.37 3.49 0.007 | O | | | | 0.86 16.750 3.13 3.12 0.006 | O | | | | 0.82 16.833 2.93 2.99 0.006 | O | | | | 0.81 16.917 2.77 2.78 0.006 | O | | | | 0.79 17.000 2.63 2.65 0.006 | O | | | | 0.78 17.083 2.51 2.52 0.006 | O | | | | 0.76 17.167 2.40 2.42 0.006 | O | | | | 0.75 17.250 2.31 2.33 0.005 | O | | | | 0.74 17.333 2.23 2.24 0.005 | O | | | | 0.73 17.417 2.16 2.17 0.005 | O | | | | 0.73 17.500 2.09 2.10 0.005 | O | | | | 0.72 17.583 2.03 2.04 0.005 | O | | | | 0.71 17.667 1.98 1.99 0.005 | O | | | | 0.71 17.750 1.93 1.94 0.005 | O | | | | 0.70 17.833 1.88 1.89 0.005 | O | | | | 0.70 17.917 1.84 1.85 0.005 | O | | | | 0.69 18.000 1.80 1.80 0.005 | O | | | | 0.69 18.083 1.74 1.75 0.005 |O | | | | 0.68 18.167 1.59 1.62 0.005 |O | | | | 0.67 18.250 1.47 1.48 0.005 |O | | | | 0.65 18.333 1.42 1.43 0.004 |O | | | | 0.65 18.417 1.39 1.39 0.004 |O | | | | 0.64 18.500 1.36 1.36 0.004 |O | | | | 0.64 18.583 1.33 1.34 0.004 |O | | | | 0.64 18.667 1.31 1.31 0.004 |O | | | | 0.64 18.750 1.29 1.29 0.004 |O | | | | 0.63 18.833 1.26 1.27 0.004 |O | | | | 0.63 18.917 1.24 1.24 0.004 |O | | | | 0.63 19.000 1.22 1.22 0.004 |O | | | | 0.63 19.083 1.20 1.21 0.004 |O | | | | 0.63 19.167 1.18 1.19 0.004 |O | | | | 0.62 19.250 1.17 1.17 0.004 |O | | | | 0.62 19.333 1.15 1.15 0.004 |O | | | | 0.62 19.417 1.13 1.14 0.004 |O | | | | 0.62 19.500 1.12 1.12 0.004 |O | | | | 0.62 19.583 1.10 1.10 0.004 |O | | | | 0.61 19.667 1.09 1.09 0.004 |O | | | | 0.61 19.750 1.07 1.08 0.004 |O | | | | 0.61 19.833 1.06 1.06 0.004 |O | | | | 0.61 19.917 1.05 1.05 0.004 |O | | | | 0.61 20.000 1.03 1.04 0.004 |O | | | | 0.61 20.083 1.02 1.02 0.004 |O | | | | 0.61 20.167 1.01 1.01 0.004 |O | | | | 0.61 20.250 1.00 1.00 0.004 |O | | | | 0.60 20.333 0.99 0.99 0.004 |O | | | | 0.60 20.417 0.98 0.98 0.004 |O | | | | 0.60 20.500 0.97 0.97 0.004 |O | | | | 0.60 20.583 0.96 0.96 0.004 |O | | | | 0.60 20.667 0.95 0.95 0.004 |O | | | | 0.60 20.750 0.94 0.94 0.004 |O | | | | 0.60 20.833 0.93 0.93 0.004 |O | | | | 0.60 20.917 0.92 0.92 0.004 |O | | | | 0.60 21.000 0.91 0.91 0.004 |O | | | | 0.59 21.083 0.90 0.90 0.004 |O | | | | 0.59 21.167 0.89 0.90 0.004 O | | | | 0.59 21.250 0.89 0.89 0.004 O | | | | 0.59 21.333 0.88 0.88 0.004 O | | | | 0.59 21.417 0.87 0.87 0.004 O | | | | 0.59 21.500 0.86 0.86 0.004 O | | | | 0.59 21.583 0.86 0.86 0.004 O | | | | 0.59 21.667 0.85 0.85 0.004 O | | | | 0.59 21.750 0.84 0.84 0.004 O | | | | 0.59 21.833 0.84 0.84 0.004 O | | | | 0.59 21.917 0.83 0.83 0.004 O | | | | 0.59 22.000 0.82 0.82 0.004 O | | | | 0.59 22.083 0.82 0.82 0.004 O | | | | 0.58 22.167 0.81 0.81 0.004 O | | | | 0.58 22.250 0.80 0.80 0.004 O | | | | 0.58 22.333 0.80 0.80 0.004 O | | | | 0.58 22.417 0.79 0.79 0.004 O | | | | 0.58 22.500 0.79 0.79 0.004 O | | | | 0.58 22.583 0.78 0.78 0.004 O | | | | 0.58 22.667 0.78 0.78 0.004 O | | | | 0.58 22.750 0.77 0.77 0.004 O | | | | 0.58 22.833 0.76 0.77 0.004 O | | | | 0.58 22.917 0.76 0.76 0.004 O | | | | 0.58 23.000 0.75 0.76 0.004 O | | | | 0.58 23.083 0.75 0.75 0.004 O | | | | 0.58 23.167 0.74 0.75 0.004 O | | | | 0.58 23.250 0.74 0.74 0.004 O | | | | 0.58 23.333 0.73 0.74 0.004 O | | | | 0.58 23.417 0.73 0.73 0.004 O | | | | 0.58 23.500 0.73 0.73 0.004 O | | | | 0.58 23.583 0.72 0.72 0.004 O | | | | 0.57 23.667 0.72 0.72 0.004 O | | | | 0.57 23.750 0.71 0.71 0.004 O | | | | 0.57 23.833 0.71 0.71 0.004 O | | | | 0.57 23.917 0.70 0.70 0.004 O | | | | 0.57 24.000 0.70 0.70 0.004 O | | | | 0.57 24.083 0.63 0.65 0.004 O | | | | 0.57 24.167 0.31 0.37 0.003 O | | | | 0.54 24.250 0.06 0.08 0.003 O | | | | 0.51 24.333 0.01 0.01 0.003 O | | | | 0.50 24.417 0.00 0.00 0.003 O | | | | 0.50 24.500 0.00 0.00 0.003 O | | | | 0.50 Remaining water in basin = 0.00 (Ac.Ft) ****************************HYDROGRAPH DATA**************************** Number of intervals = 294 Time interval = 5.0 (Min.) Maximum/Peak flow rate = 20.070 (CFS) Total volume = 3.152 (Ac.Ft) Status of hydrographs being held in storage Stream 1 Stream 2 Stream 3 Stream 4 Stream 5 Peak (CFS) 0.000 0.000 0.000 0.000 0.000 Vol (Ac.Ft) 0.000 0.000 0.000 0.000 0.000 *********************************************************************** ‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐‐ Project Description Friction Method Manning Formula Solve For Discharge Input Data Roughness Coefficient 0.013 Channel Slope 0.03650 ft/ft Normal Depth 0.50 ft Diameter 1.50 ft Discharge 4.81 ft³/s Cross Section Image 18" Outlet @d=0.5' 12/15/2022 12:04:25 PM Bentley Systems, Inc. Haestad Methods Solution CenterBentley FlowMaster V8i (SELECTseries 1) [08.11.01.03] 27 Siemons Company Drive Suite 200 W Watertown, CT 06795 USA +1-203-755-1666 1of1Page Project Description Friction Method Manning Formula Solve For Full Flow Capacity Input Data Roughness Coefficient 0.013 Channel Slope 0.03650 ft/ft Normal Depth 1.50 ft Diameter 1.50 ft Discharge 20.07 ft³/s Results Discharge 20.07 ft³/s Normal Depth 1.50 ft Flow Area 1.77 ft² Wetted Perimeter 4.71 ft Hydraulic Radius 0.38 ft Top Width 0.00 ft Critical Depth 1.47 ft Percent Full 100.0 % Critical Slope 0.03259 ft/ft Velocity 11.36 ft/s Velocity Head 2.00 ft Specific Energy 3.50 ft Froude Number 0.00 Maximum Discharge 21.59 ft³/s Discharge Full 20.07 ft³/s Slope Full 0.03650 ft/ft Flow Type SubCritical GVF Input Data Downstream Depth 0.00 ft Length 0.00 ft Number Of Steps 0 GVF Output Data Upstream Depth 0.00 ft Profile Description Profile Headloss 0.00 ft Average End Depth Over Rise 0.00 % 18" Outlet @full 12/15/2022 1:40:00 PM Bentley Systems, Inc. Haestad Methods Solution CenterBentley FlowMaster V8i (SELECTseries 1) [08.11.01.03] 27 Siemons Company Drive Suite 200 W Watertown, CT 06795 USA +1-203-755-1666 2of1Page GVF Output Data Normal Depth Over Rise 100.00 % Downstream Velocity Infinity ft/s Upstream Velocity Infinity ft/s Normal Depth 1.50 ft Critical Depth 1.47 ft Channel Slope 0.03650 ft/ft Critical Slope 0.03259 ft/ft 18" Outlet @full 12/15/2022 1:40:00 PM Bentley Systems, Inc. Haestad Methods Solution CenterBentley FlowMaster V8i (SELECTseries 1) [08.11.01.03] 27 Siemons Company Drive Suite 200 W Watertown, CT 06795 USA +1-203-755-1666 2of2Page Project Description Friction Method Manning Formula Solve For Discharge Input Data Roughness Coefficient 0.013 Channel Slope 0.03650 ft/ft Normal Depth 1.00 ft Diameter 1.50 ft Discharge 15.73 ft³/s Cross Section Image 18" Outlet @d=1' 12/15/2022 1:39:04 PM Bentley Systems, Inc. Haestad Methods Solution CenterBentley FlowMaster V8i (SELECTseries 1) [08.11.01.03] 27 Siemons Company Drive Suite 200 W Watertown, CT 06795 USA +1-203-755-1666 1of1Page APPENDIX G SOIL REPORT EXCERPTS 6634 Valjean Avenue, Van Nuys, California 91406 Phone: (818) 785-2158 Fax: (818) 785-1548 MDN 23013A GEOLOGIC AND GEOTECHNICAL ENGINEERING INVESTIGATION REPORT, PROPOSED SFD RESIDENTIAL DEVELOPMENT, North Corner of Chase Road & Aria Lane, Fontana, California for Ridge Crest Real Estate, LLC July 19, 2022 W.O. 7726 (Revised July 28, 2022) 6634 Valjean Avenue, Van Nuys, California 91406 Phone: (818) 785-2158 Fax: (818) 785-1548 MDN 23013A July 19, 2022 W.O. 7726 (Revised July 28, 2022) RIDGE CREST REAL ESTATE, LLC 353 E. Angeleno Avenue A, Burbank, California 91502 Attention: Mr. Timothy Sales Subject: Geologic and Geotechnical Engineering Investigation Report, Proposed SFD Residential Development, North Corner of Chase Road & Aria Lane, Fontana, California As requested, GeoSoils Consultants, Inc. (GSC) has performed a geologic and geotechnical engineering investigation on the subject tract. The purpose of this investigation is to provide geologic and geotechnical engineering recommendations for site grading and foundations. The report presents the results of our research, subsurface exploration, laboratory testing, site reconnaissance, and provides geotechnical engineering recommendations for site grading. Grading of the site is considered feasible from a geologic and geotechnical engineering prospective, provided the recommendations presented herein are incorporated into the design and implemented during grading. We appreciate this opportunity to be of service to you. If you have any questions regarding this report, or if we may be of further assistance to you, please do not hesitate to contact us. Very truly yours, GEOSOILS CONSULTANTS, INC. MAHAN PASDARPOUR RUDY F. RUBERTI PE 90111 CEG 1708 cc: (1) Addressee Page 25 July 19, 2022 W.O. 7726 (Revised July 28, 2022) MDN 23013A TABLE 5 PERCOLATION TEST RESULTS Test Location Percolation Depth (ft) Pre-Adjusted Rate (inch/hour) * B-6 10-15 15.24 B-7 20-30 2.29 B-8/P-1 30-40 2.62 B-9/P-2 40-50 11.73 *Reduction factor should be applied by the Civil Engineer of The Record It is our professional opinion that on-site infiltration will not be a hazard to the potential development and the site is suitable for storm water infiltration. The proposed infiltration rates were calculated in inches per hour and are without factor of safety. Per our discussion with the civil engineer of the record, Mr. Anthony Ng from United Civil Inc, it is our understanding that the civil engineer will apply an appropriate factor of safety to these infiltration rates to calculate dry wells design percolation rates. 6.6 Corrosion Characteristics of Soil As a screening level study, limited chemical and electrical tests were performed on samples considered representative of the onsite soils to identify potential corrosive characteristics of these soils. The common indicators that are generally associated with soil corrosivity, among other indicators, include water-soluble sulfate (a measure of soil corrosivity on concrete), water-soluble chloride (a measure of soil corrosivity on metals embedded in concrete), pH (a measure of soil acidity), and minimum electrical resistivity (a measure of corrosivity on metals embedded in soils). Test methodology and results are presented in Appendix B. It should be noted that GeoSoils does not practice corrosion engineering; therefore, the test results, opinion and engineering judgment provided herein should be considered as general guidelines only. Additional analyses, and/or determination of other indicators, would be warranted, especially, for cases where buried metallic building materials (such as copper and cast or ductile iron pipes) in contact with site B-3B-7 B-1B-5 B-6 B-4 B-8/P-1 B-9/P-2 B-2 B-3B-7 B-6 B-4 B-8/P-1 B-9/P-2 EXPLANATION APPROXIMATE LOCATION OF BORINGB-7 WORK ORDER DATE SCALE REVISED PLATE 1 6634 Valjean Avenue Van Nuys, CA 91406 GEOTECHNICAL GEOLOGIC ENVIRONMENTAL GeoSoils Consultants Inc.GSC 7726 7/2022 1" = 30' PROPOSED RESIDENTIAL DEVELOPMENT NORTH CORNER OF CHASE ROAD & ARIA LANE FONTANA, CALIFORNIA RIDGECREST REAL ESTATE, LLC. MDN 23013A P-2 APPROXIMATE LOCATION OF PERCOLATION TEST X: \ 2 0 0 1 w . o \ g s c - c a d \ 7 7 2 6 \ 5 - 9 - 2 2 \ C U R R E N T \ P l a t e 1 . d w g , 7 / 2 8 / 2 0 2 2 3 : 1 7 : 4 4 P M , A u t o C A D P D F ( H i g h Q u a l i t y P r i n t ) . p c 3 APPENDIX H DESIGN CAPTURE VOLUME (DCV) CALCULATION Water Quality Management Plan (WQMP) 4‐8 4.2 Project Performance Criteria The purpose of this section of the Project WQMP is to establish targets for post‐development hydrology based on performance criteria specified in the MS4 Permit. These targets include runoff volume for water quality control (referred to as LID design capture volume), and runoff volume, time of concentration, and peak runoff for protection of any downstream waterbody segments with a HCOC. If the project has more than one outlet for stormwater runoff, then complete additional versions of these forms for each DA / outlet. Methods applied in the following forms include: For LID BMP Design Capture Volume (DCV), the San Bernardino County Stormwater Program requires use of the P6 method (MS4 Permit Section XI.D.6a.ii) – Form 4.2‐1 For HCOC pre‐ and post‐development hydrologic calculation, the San Bernardino County Stormwater Program requires the use of the Rational Method (San Bernardino County Hydrology Manual Section D). Forms 4.2‐2 through Form 4.2‐5 calculate hydrologic variables including runoff volume, time of concentration, and peak runoff from the project site pre‐ and post‐development using the Hydrology Manual Rational Method approach. For projects greater than 640 acres (1.0 mi2), the Rational Method and these forms should not be used. For such projects, the Unit Hydrograph Method (San Bernardino County Hydrology Manual Section E) shall be applied for hydrologic calculations for HCOC performance criteria. Refer to Section 4 in the TGD for WQMP for detailed guidance and instructions. Form 4.2‐1 LID BMP Performance Criteria for Design Capture Volume (DA 1) 1 Project area DA 1 (ft2): 297,939 2 Imperviousness after applying preventative site design practices (Imp%): 65 3 Runoff Coefficient (Rc): _0.339 Rc = 0.858(Imp%)^3‐0.78(Imp%)^2+0.774(Imp%)+0.04 4 Determine 1‐hour rainfall depth for a 2‐year return period P2yr‐1hr (in): 0.655 http://hdsc.nws.noaa.gov/hdsc/pfds/sa/sca_pfds.html 5 Compute P6, Mean 6‐hr Precipitation (inches): 0.97 P6 = Item 4 *C1, where C1 is a function of site climatic region specified in Form 3‐1 Item 1 (Valley = 1.4807; Mountain = 1.909; Desert = 1.2371) 6 Drawdown Rate Use 48 hours as the default condition. Selection and use of the 24 hour drawdown time condition is subject to approval by the local jurisdiction. The necessary BMP footprint is a function of drawdown time. While shorter drawdown times reduce the performance criteria for LID BMP design capture volume, the depth of water that can be stored is also reduced. 24‐hrs 48‐hrs 7 Compute design capture volume, DCV (ft3): 21,232 DCV = 1/12 * [Item 1* Item 3 *Item 5 * C2], where C2 is a function of drawdown rate (24‐hr = 1.582; 48‐hr = 1.963) Compute separate DCV for each outlet from the project site per schematic drawn in Form 3‐1 Item 2 L= 8 3 7 ' A A = 6.84 AC Q = 14.84 CFS NOT A PART NOT A PART NOT A PART NOT A PART 100 PL PL PL PL IN THE CITY OF FONTANA, STATE OF CALIFORNIA EXISTING HYDROLOGY MAP TRACT NO. 20580 L=573' B A Q100 TRACT 20580 FONTANA, CA PREPARED BY: UNITED CIVIL, INC. 30141 AGOURA ROAD, SUITE 215 AGOURA HILLS, CA 91301 PH: (818) 707-8648 FAX: (818) 707-8649 RC HOMES, INC. DEVELOPER/APPLICANT:DRAINAGE MAP RIDGE CREST REAL ESTATE, LLC LOS ANGELES, CA 90004 550 N LARCHMONT BLVD., SUITE 201 PRE DEVELOPED CONDITION TEL: (323) 450-2334 Site NO S C A L E VICINITY MAP ONT A R I O F W Y FOOTHILL FWY W FOOTHILL BLVD SI E R R A A V E SAN BERNARDINO FWY BASELINE AVE SD SD SD SD SD SD SD SD SD SD SD SD SD SD D D D A A = 3.43 AC Q = 13.74 CFS B A = 1.79 AC Q = 8.46 CFS C A = 1.62 AC Q = 7.96 CFS 100 100 100 PL PL PL PL TRENCH W/ 72" DIAM. PROP. DETENTION CASCADE DRIVE "A " D R I V E "B " D R I V E "D " D R I V E "C" DRIVE CMP PIPE (94'X8'X7') TRENCH W/ 84" DIAM. PROP. INFILTRATION PERFORATED CMP PIPE (79'X39'X8') Q100 (ALLOWABLE)=20.07 CFS Q100 (DESIGN)=20.07 CFS IN THE CITY OF FONTANA, STATE OF CALIFORNIA PROPOSED HYDROLOGY MAP TRACT NO. 20580 TRACT 20580 FONTANA, CA PREPARED BY: UNITED CIVIL, INC. 30141 AGOURA ROAD, SUITE 215 AGOURA HILLS, CA 91301 PH: (818) 707-8648 FAX: (818) 707-8649 RC HOMES, INC. DEVELOPER/APPLICANT:DRAINAGE MAP RIDGE CREST REAL ESTATE, LLC LOS ANGELES, CA 90004 550 N LARCHMONT BLVD., SUITE 201 POST DEVELOPED CONDITION TEL: (323) 450-2334 B A Q100 Site NO S C A L E VICINITY MAP ONT A R I O F W Y FOOTHILL FWY W FOOTHILL BLVD SI E R R A A V E SAN BERNARDINO FWY BASELINE AVE UNDERGROUND INFILTRATION SYSTEM - TRENCH WITH 84" DIAMETER PERFORATED PIPE APPENDIX H HYDROLOGY MAPS Tract No. 20580 Fontana, CA