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Published byJonah Quinn Modified over 8 years ago
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Hydrologic Calibration: October 2010 U PDATE OF E FFECTIVE H YDROLOGY FOR M ARYS C REEK
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Agenda Background Hydrologic model Hydrologic calibration 100-year discharges, Existing Conditions
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Background Largest contributor to the Clear Fork of Trinity River 55.2 mi 2 Drainage area of Clear Fork at the confluence is 8.5 mi 2
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Aerial View Marys Creek Clear Fork Trinity River
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100-year Floodplain Marys Creek Clear Fork Trinity River
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DFIRM
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Effective WSEL Profile Marys Creek Clear Fork of Trinity River
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Effective Hydrology Used NuDallas 37 subbasins 15-min time step Initial and constant loss Snyder’s UH Location Drainage Area (mi2) 100-yr Discharge (cfs) Marys Creek At Confluence56.04 42,800 Clear Fork Upstream of Confluence 8.513,000 Downstream of Confluence 63.2 25,400 FIS
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Purpose of Study Update the flows on Marys Creek and the Clear Fork of the Trinity River. Phase I Create a new hydraulic model to analyze the confluence of Marys Creek with the Clear Fork. Phase II Remap the 100-year floodplain at the confluence
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Hydrologic Model HEC-HMS 49 basins Routing – Modified Puls (main streams) – Muskingum Cunge (smaller streams) Losses and Unit Hydrographs – Initial and constant with Snyder’s U.H. – Curve Number and SCS U.H. 5-minutes time step
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Subbasins
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Historical Events, June 2000
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Historical Events, June 2004
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Historical Events, March 2007
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Calibrated Rainfall
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USGS Gage, Rating Curve Based on field measurements up to a stage of 6 feet Extrapolated above 6 feet
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USGS Gage, Rating Curve
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Adjusted Discharges, June 2000
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Adjusted Discharges, June 2004
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Adjusted Discharges, March 2007
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Hydrologic Calibration Adjust hydrologic model to match the observed (adjusted) discharges Match basin response by adjusting – Infiltration losses – lag times Very time consuming
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Calibration
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Hydrologic Calibration, June 2000
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Hydrologic Calibration, June 2004
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Hydrologic Calibration, March 07
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Frequency Events Snyder’s – Average lag times – Average constant losses – Initial loss: 2 inches SCS – Average lag times – CN (II) – Initial loss: default (0.2S) Frequency Rainfall – ISWMM (USGS)
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100-year, Existing Conditions
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Flow Comparison FIS: 42,800 cfs Snyder’s: 31,700 cfs SCS: 31,200 cfs
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Summary More accurate hydrology for Marys Creek based on calibration of 3 historical events Lowered peak discharges by about 25%
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Questions
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