Filters: Tags: Peak discharge (X)
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Categories: Publication;
Types: Citation;
Tags: *RAINFALL-RUNOFF RELATIONSHIPS,
*URBANIZATION,
*WATER POLLUTION SOURCES,
CITIES,
EROSION,
Categories: Publication;
Types: Citation;
Tags: Flood frequency,
Flood hydrographs,
Floods,
Gaging stations,
Hydraulic design,
Categories: Publication;
Types: Citation;
Tags: Arid climate,
Climatology,
EE 444.1 Surface Water; EE 442.1 Flood Control; EE 921.6 Num,
Environmental Engineering Abstracts,
Estimation,
Categories: Publication;
Types: Citation;
Tags: SW 0835 Streamflow and runoff,
USA, Tennessee,
Water Resources Abstracts,
catchment areas,
flood frequency,
Categories: Publication;
Types: Citation;
Tags: Flood forecasting,
Flooding,
Hawaii,
Peak discharge,
Rainfall-runoff relationships,
Extreme floods often follow wildfire in mountainous watersheds. However, a quantitative relation between the runoff response and burn severity at the watershed scale has not been established. Runoff response was measured as the runoff coefficient C, which is equal to the peak discharge per unit drainage area divided by the average maximum 30 min rainfall intensity during each rain storm. The magnitude of the burn severity was expressed as the change in the normalized burn ratio. A new burn severity variable, hydraulic functional connectivity Φ was developed and incorporates both the magnitude of the burn severity and the spatial sequence of the burn severity along hillslope flow paths. The runoff response and the...
Categories: Publication;
Types: Citation;
Tags: Burn severity,
connectivity,
peak discharge,
runoff r
Extreme floods often follow wildfire in mountainous watersheds. However, a quantitative relation between the runoff response and burn severity at the watershed scale has not been established. Runoff response was measured as the runoff coefficient C, which is equal to the peak discharge per unit drainage area divided by the average maximum 30 min rainfall intensity during each rain storm. The magnitude of the burn severity was expressed as the change in the normalized burn ratio. A new burn severity variable, hydraulic functional connectivity Φ was developed and incorporates both the magnitude of the burn severity and the spatial sequence of the burn severity along hillslope flow paths. The runoff response and the...
Categories: Publication;
Types: Citation;
Tags: Burn severity,
connectivity,
peak discharge,
runoff r
Categories: Publication;
Types: Citation;
Tags: *FLOOD FREQUENCY,
*STORM RUNOFF,
*URBAN HYDROLOGY,
*URBAN RUNOFF,
*VIRGINIA,
Categories: Publication;
Types: Citation;
Tags: Flood frequency,
Floods,
Historic flood,
Peak discharge,
Precipitation,
Categories: Publication;
Types: Citation;
Tags: *RAINFALL-RUNOFF RELATIONSHIPS,
*STORM RUNOFF,
*TULSA(OKLA),
*UNIT HYDROGRAPHS,
*URBAN HYDROLOGY,
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