cbrfc flash flood support
DESCRIPTION
CBRFC Flash Flood Support. Many channels and dry washes duplicate as high use recreational trails. Due in part to the varied terrain and soil types flash floods are not constricted to existing channels. Western Region Flash Flood Factors. - PowerPoint PPT PresentationTRANSCRIPT
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CBRFC Flash Flood Support
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Flash floods are generally localized, short-duration events associated with heavy rain.
Western Region Flash Flood Factors . . .
Precipitation intensity, basin geography and physiographic features have greater influence than antecedent soil moisture.
Why the CBRFC uses a customized method…
Flash floods frequently occur in small basins generally less than 20 square miles in size.
Flash floods occur rapidly, frequently on at time scale less than 1 hour.
SAC-SMA calibrated basins are much larger in size than flash flood basins.
SAC-SMA operates on time scales much greater than the flash flood time scale.
It is very difficult to determine a critical flash flood flow/stage level required by earlier methods
Many channels and dry washes duplicate as high use recreational trails.
Due in part to the varied terrain and soil types flash floods are not constricted to existing channels.
SAC-SMA calibrations do not exist across the entire RFC area.
Due to the limitations listed – FFG using SAC-SMA requires significant modification.
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Colorado Basin
Rules of thumb – skewed and given spatial variability based on the GIS generated flash flood potential index (FFPI).
California - Nevada
Rules of thumb – skewed and given spatial variability based on the GIS generated flash flood potential index (FFPI)
Northwest
Geospatial analysis of known flash flood events used to create a GIS model for computing FFG
Western Region RFC gridded FFG Generation Methods:
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Soil type
The Flash Flood Potential Index uses information such as land-use, forest density, slope, and soil type to characterize an areas potential response to heavy rainfall
Vegetation type and density
Slopes
?
Land Use
Cedar City, UTFFMP Radar Basins
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3
7
8
8
3
7
8
46
9
69
Slope
Forest Density
Land Use
Soil
Flash Flood Potential Index
1 10
Greater response and potential
Lesser response and potential
FFPI MethodCreating a single FFPI layer
Hydrologic response
56
8
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FFPI in a Gridded Format
East Fork of the Virgin River
Southwest Utah
Decreasing Potential
Increasing Potential
FFPI
1
10
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The FFPI values range from 1 to 9 with a mean value for the CBRFC near 4
If FFPI = 4: FFG is 1.00
If FFPI = 5: FFG is .90
If FFPI = 6: FFG is . 80
If FFPI = 7: FFG is .70
if FFPI = 8: FFG is .60
if FFPI = 9: FFG is .55
if FFPI = 3: FFG is 1.45
if FFPI = 2: FFG is 2.00
if FFPI = 1: FFG is 2.25
CBRFC FFPI / FFG Relationship:
• Start with reasonable average FFG values of – 1 inch in 1 hour
• Assign these values to grid cells with the mean FFPI value of 4• Incrementally adjust the FFG values up or down as FFPI varies• Limit the range of FFG values to climatologically reasonable values• Verify results by comparing to archived flash flood events & modify
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FFG Grid Modified by FFPI
1.0 per 1 hour 1.0
1.5
0.9
0.7
2.3
1.0
0.8
0.6
0.7
FFPI Grid Gridded FFG product for FFMP
If the mean FFPI value for the entire RFC area is 4 thus all FFPI grid boxes of “4” will get assigned the value for the pertinent time period. Other values are scaled up or down by a selected range.
4 4
1
7
75 6
8
Initialize FFG Grid Cell
3
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CBRFC FFG Summary:
Outputs:
1, 3, 6, hour gridded guidance provided to FFMP and D2D
Gridded FFG that is modulated by the FFPI for input into the FFMP
Inputs:
Rule of thumb – 1 inch per hour as a starting point
Gridded FFPI - Used to adjust FFG on a grid-cell by grid-cell basis to create greater spatial resolution in FFG and account for physiographic characteristics.
Use:
Direct use through FFMP - Gridded FFG that uses FFPI Information
Stand alone FFPI (D2D, or GIS display package) in a qualitative manner
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CBRFC Flash Flood Guidance Influenced by the Flash Flood Potential Index
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Non-Exceedance
values
Grid of Discharge or Surface Flow
Future Operational Concept:
Strategy: Model flash floods via hydrologic model
CriticalThreshold
“The current discharge is in the top 5% of historical responses…”
DischargeOrSurfaceFlow
Fre
quen
cy
DHM-FSR Post- Processor
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Frequency Discharge ExampleDischarge FrequencyDischarge
Non Exceedance Percentage
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Frequency Surface Flow ExampleSurface Flow FrequencySurface Flow
Non Exceedence Percentage
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Summary
• CBRFC flash flood guidance based on static FFPI grids
• Possible to modify for wildfire
• Future concept based on distributed hydrologic model; prototyping work at OHD