THE EFFECT OF MODEL CONFIGURATION ON MODELLED HILLSLOPE-RIPARIAN INTERACTIONS

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dc.contributor.author Cloke H.L.
dc.contributor.author Renaud J.P.
dc.contributor.author Claxton A.J.
dc.contributor.author McDonnell J.J.
dc.contributor.author Anderson M.G.
dc.contributor.author Blake J.R.
dc.contributor.author Bates P.D.
dc.date.accessioned 2022-01-26T02:46:31Z
dc.date.available 2022-01-26T02:46:31Z
dc.date.issued 2003
dc.identifier https://elibrary.ru/item.asp?id=5055505
dc.identifier.citation Journal of Hydrology, 2003, 279, 1-4, 167-181
dc.identifier.issn 0022-1694
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/34607
dc.description.abstract The transfer of hillslope water to and through the riparian zone forms a research area of importance in hydrological investigations. Numerical modelling schemes offer a way to visualise and quantify first-order controls on catchment runoff response and mixing. We use a two-dimensional Finite Element model to assess the link between model setup decisions (e.g. zero-flux boundary definitions, soil algorithm choice) and the consequential hydrological process behaviour. A detailed understanding of the consequences of model configuration is required in order to produce reliable estimates of state variables. We demonstrate that model configuration decisions can determine effectively the presence or absence of particular hillslope flow processes and, the magnitude and direction of flux at the hillslope-riparian interface. If these consequences are not fully explored for any given scheme and application, the resulting process inference may well be misleading.
dc.subject HILLSLOPE HYDROLOGY
dc.subject FINITE ELEMENT MODELLING
dc.subject BOUNDARY CONDITIONS
dc.subject RIPARIAN ZONE
dc.title THE EFFECT OF MODEL CONFIGURATION ON MODELLED HILLSLOPE-RIPARIAN INTERACTIONS
dc.type Статья


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