Where does water go when it rains? Moving beyond the variable source area concept of rainfall‐runoff response
- 20 June 2003
- journal article
- invited commentary
- Published by Wiley in Hydrological Processes
- Vol. 17 (9), 1869-1875
- https://doi.org/10.1002/hyp.5132
Abstract
No abstract availableThis publication has 20 references indexed in Scilit:
- Groundwater dynamics along a hillslope: A test of the steady state hypothesisWater Resources Research, 2003
- The role of bedrock topography on subsurface storm flowWater Resources Research, 2002
- On the dialog between experimentalist and modeler in catchment hydrology: Use of soft data for multicriteria model calibrationWater Resources Research, 2002
- Estimation of baseflow residence times in watersheds from the runoff hydrograph recession: method and application in the Neversink watershed, Catskill Mountains, New YorkHydrological Processes, 2002
- The zone of vegetation influence on baseflow revealed by diel patterns of streamflow and vegetation water use in a headwater basinHydrological Processes, 2002
- Process‐oriented catchment modelling and multiple‐response validationHydrological Processes, 2002
- Base cation concentrations in subsurface flow from a forested hillslope: The role of flushing frequencyWater Resources Research, 1998
- Hydrologic response of a steep, unchanneled valley to natural and applied rainfallWater Resources Research, 1997
- Relation of field studies and modeling in the prediction of storm runoffJournal of Hydrology, 1983
- River flow forecasting through conceptual models part I — A discussion of principlesJournal of Hydrology, 1970