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- W568021281 abstract "The hydrological response of catchments is influenced by the lanscape characteristics. Both channel networks and hillslopes play a major role in the propagation of water within catchments, and therefore influence the generation of floods. In mountainous regions, the importance of subsurface flows has been recognized for a long time (e.g. Dunne and Black 1970, Freeze 1972a, Beven and Kirkby 1979). Moreover, the issue of hydrological modeling or forecasting in a context of poorly or ungauged basins adds a level of complexity by removing the possibility to calibrate hydrological models. In this report, we focus on the subsurface component of discharge at the hillslope scale (up to one km2), and in particular on the development of a new approach providing the ability to capture the essential behaviour of the natural system using a parsimonious and computational efficient modeling. The report first presents a theoretical analysis of subsurface flow for complex hillslopes (Chapter 2 and Chapter 3), and then the first results of its application to real catchments (Chapter 4)." @default.
- W568021281 created "2016-06-24" @default.
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- W568021281 date "2007-04-17" @default.
- W568021281 modified "2023-09-27" @default.
- W568021281 title "Hill-slope Hydrological Model for Flash Flood" @default.
- W568021281 hasPublicationYear "2007" @default.
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