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Approximate Floodplain Mapping - Procedures and Approaches to Data Challenges Troy Thielen, CFM Brett Addams, CFM May 18, 2010
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Procedures and Approaches to Data Challenges Overview 1. Approximate Floodplain Mapping Defined 2. Study Area 3. Procedure/Methodology 4. Challenges Encountered
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Approximate Study – Zone A DFIRM
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Challenges Encountered in Flat Terrain Case Study: Northwest Ohio’s Black Swamp region Source: Ohio History Central
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Challenges Encountered in Flat Terrain Methodology 1. Hydrology 2. Hydraulics 3. Mapping
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Hydrology u Flows calculated using USGS Regression Equations u Input parameters calculated by using ArcHydro, via StreamStats
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295.0232.0 8510 757.0 100 )1(*)(*)(*)( WSLDARC 100 = Peak flow for a 100-yr recurrence interval RC DA 8510 SL W = Regression constant (dependent on project location) = Drainage area (sq. miles) = Slope = Open water or wetlands (percentage of drainage area) USGS Regression Equation Hydrology
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http://water.usgs.gov/osw/streamstats/ssonline.html StreamStats Web-based application that computes streamflow statistics for both gaged and ungaged sites. Includes a map-based user interface that uses ArcIMS, ArcSDE, ArcGIS and ArcHydro. Hydrology
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Hydrology StreamStats
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Hydrology
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Hydrology StreamStats Shapefiles
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Vector Stream Network Digital Elevation ModelHydrology ArcHydro Inputs
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Hydraulics u Hydraulic Model: HEC-RAS u HEC-GeoRAS extension of ArcGIS used for pre- and post-processing GIS inputs u Process: 1. Pre-processing of GIS Data 2. Import to HEC-RAS 3. HEC-RAS modeling 4. Export HEC-RAS data to GIS
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Hydraulics Cutting Cross-sections
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Hydraulics Channel Manually Added to XS Geometry
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Model Input - Stream Centerline - Flowpaths - XS Cut Lines Model Output - Bounding Polygons - Floodplain Boundaries (bp001) - XS Cut Lines Terrain Grid Depth Grid Water Surface Grid Hydraulics
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Mapping u Post-Processing of raw GeoRAS floodplain polygon output u Review for accuracy u Clean up data anomalies u Adjust mapping to meet FEMA standards
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Mapping Post-Processing
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Challenges Encountered in Flat Terrain u Hydrology – difficulty in defining drainage divides and flow paths u Hydraulics – Floodplain outputs may indicate need for model corrections u Island and Ponds – Segmented floodplain outputs require further analysis u Lateral Flow Areas – Flat terrain can artificially amplify flooding effects
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Challenges Encountered in Flat Terrain Challenge: Hydrology u Automated delineation of hydrologic features can result in erroneous results u Analysis and manual correction is required
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Challenge: Hydrology Basin Delineation
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Challenge: Hydrology Ditch Network
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Challenges Encountered in Flat Terrain Challenge: Hydraulics u Analysis of floodplain outputs may require review of modeling data
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Challenge: Hydraulics Raw HEC-GeoRAS output
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Challenge: Hydraulics Model Run 1
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Challenge: Hydraulics Model Run 2
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Challenge: Hydraulics Run 1 vs. Run 2
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Challenges Encountered in Flat Terrain Challenge: ISLANDS and PONDS u Very minor terrain variation can result in numerous islands and disconnected ponds u Result: –Highly segmented floodplain output generated
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Challenge: Islands and Ponds Raw HEC-GeoRAS Output
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Depth Grids Subtract Ground DEM values from Water Surface DEM values
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Depth Grids Depth Grid – Stretched
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Depth Grids Depth Grid – Classified Values
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Challenge: Islands and Ponds Islands only slightly above the calculated WSEL
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Challenge: Islands and Ponds Disconnected ponds at very shallow depth
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Challenges Encountered in Flat Terrain Challenge: LATERAL FLOW AREAS u Unreasonable split flow situations u Unreasonably large flooding effects along portions of the floodplain
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Challenge: Lateral Flow Areas Raw HEC-GeoRAS Output
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Challenge: Lateral Flow Areas
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Conclusion Troy Thielen, CFM thielentr@cdm.com Brett Addams, CFM addamsbh@cdm.com (312) 346-5000 Questions
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