Casper, Wyoming
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Accounting, transit losses, instream flows
Watershed to continental-scale models
Terrain, land cover, ET, spatial data
Previous study · Continental-scale forecasting
Forecast weather and streamflow models account for uncertainty by utilizing multi-member ensembles. Utilizing each member of the weather ensemble, flow models translate weather information into multiple streamflow simulations for each stream reach. However, when flood maps are generated only a single flow rate is chosen for each stream reach and a single flood map is generated. The emphasis of this project is to develop a methodology to create ensemble flood maps for use in continental-scale forecasting frameworks. In so doing, uncertainty in weather/flow forecasts can be realized through the differences in expected flood extents.
The figure shows the method for generating operational (forecast) flood maps using flow rates from a 21-member ensemble. Dark-blue shows agreement between all of the flood ensemble members. Light blue indicates where only some of the ensemble members indicate flooding to occur.
Why it matters: a flood forecast shows not just where water may go, but how sure the forecast is.
Project facts
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