On the generation of delayed peaks in stream discharge
Where deep permeable soils overlie impermeable bedrock and where steep hillslopes border a narrow floodplain, subsurface stormflow dominates the hydrograph. In such cases delayed peaks in stream discharge may occur several days after rainfall, providing the major volumetric response and possibly als...
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Published in | Journal of hydrology (Amsterdam) Vol. 78; no. 3; pp. 361 - 378 |
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Main Authors | , |
Format | Journal Article |
Language | English |
Published |
Amsterdam
Elsevier B.V
01.01.1985
Elsevier Science |
Subjects | |
Online Access | Get full text |
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