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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Bibliographic Details
Published inJournal of hydrology (Amsterdam) Vol. 78; no. 3; pp. 361 - 378
Main Authors Burt, T.P., Butcher, D.P.
Format Journal Article
LanguageEnglish
Published Amsterdam Elsevier B.V 01.01.1985
Elsevier Science
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