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Analysis of lag time (defined as time between centroids of effective precipitation and runoff) from nine small urban watersheds shows that lag time variability is small and that lag time is not correlated with storm intensity; effective precipitation can be routed through storage by Muskingum method to accurately reproduce observed runoff hydrograph; effective precipitation is separated from total precipitation by phi-index; precipitation loss on watershed is closely represented by linear relationship between total storm precipitation and total storm runoff.
Analysis of lag time (defined as time between centroids of effective precipitation and runoff) from nine small urban watersheds shows that lag time variability is small and that lag time is not correlated with storm intensity; effective precipitation can be routed through storage by Muskingum method to accurately reproduce observed runoff hydrograph; effective precipitation is separated from total precipitation by phi-index; precipitation loss on watershed is closely represented by linear relationship between total storm precipitation and total storm runoff.
Time in urban hydrology
ASCE -- Proc (J Hydraulics Div)
Willeke, G.E. (author)
1966
99 pages
Article (Journal)
English
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| ASCE | 2021
| UB Braunschweig | 1984
| TIBKAT | 1984
Discussion of “Time in Urban Hydrology”
| ASCE | 2021
Closure to “Time in Urban Hydrology”
| ASCE | 2021