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Description
  • Two conceptually different approaches to numerical modeling of a hillslope response to a rainstorm are presented and compared. In the first approach, the flow of water in a variably saturated hillslope segment is described as vertical planar flow using two-dimensional Richards' equation. Preferential flow effects are taken into account by formulating a dual set of two-dimensional governing equations, which reflects the dual character of the flow in the soil matrix and in the preferential flow domain. In the second approach, one-dimensional variably saturated vertical flow is coupled with one-dimensional saturated subsurface flow along the soil-bedrock interface. The saturated downhill flow is described by one-dimensional diffusion wave equation while the vertical flow is modeled using a dual set of one-dimensional Richards' equations.
  • Two conceptually different approaches to numerical modeling of a hillslope response to a rainstorm are presented and compared. In the first approach, the flow of water in a variably saturated hillslope segment is described as vertical planar flow using two-dimensional Richards' equation. Preferential flow effects are taken into account by formulating a dual set of two-dimensional governing equations, which reflects the dual character of the flow in the soil matrix and in the preferential flow domain. In the second approach, one-dimensional variably saturated vertical flow is coupled with one-dimensional saturated subsurface flow along the soil-bedrock interface. The saturated downhill flow is described by one-dimensional diffusion wave equation while the vertical flow is modeled using a dual set of one-dimensional Richards' equations. (en)
Title
  • Comparison of Two Different Approaches to Modeling Subsurface Runoff at the Hillslope Scale
  • Comparison of Two Different Approaches to Modeling Subsurface Runoff at the Hillslope Scale (en)
skos:prefLabel
  • Comparison of Two Different Approaches to Modeling Subsurface Runoff at the Hillslope Scale
  • Comparison of Two Different Approaches to Modeling Subsurface Runoff at the Hillslope Scale (en)
skos:notation
  • RIV/68407700:21110/06:00125053!RIV14-GA0-21110___
http://linked.open...avai/riv/aktivita
http://linked.open...avai/riv/aktivity
  • P(GA205/05/2312)
http://linked.open...vai/riv/dodaniDat
http://linked.open...aciTvurceVysledku
http://linked.open.../riv/druhVysledku
http://linked.open...iv/duvernostUdaju
http://linked.open...titaPredkladatele
http://linked.open...dnocenehoVysledku
  • 469331
http://linked.open...ai/riv/idVysledku
  • RIV/68407700:21110/06:00125053
http://linked.open...riv/jazykVysledku
http://linked.open.../riv/klicovaSlova
  • hillslope scale; subsurface runoff (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...ontrolniKodProRIV
  • [DB72E387AE2E]
http://linked.open...v/mistoKonaniAkce
  • Vídeň
http://linked.open...i/riv/mistoVydani
  • Strasbourg Ceres
http://linked.open...i/riv/nazevZdroje
  • Geophysical Research Abstracts: Volume 8, 2006
http://linked.open...in/vavai/riv/obor
http://linked.open...ichTvurcuVysledku
http://linked.open...cetTvurcuVysledku
http://linked.open...vavai/riv/projekt
http://linked.open...UplatneniVysledku
http://linked.open...iv/tvurceVysledku
  • Dušek, Jaromír
  • Vogel, Tomáš
http://linked.open...vavai/riv/typAkce
http://linked.open.../riv/zahajeniAkce
issn
  • 1029-7006
number of pages
http://purl.org/ne...btex#hasPublisher
  • European Geosciences Union
http://localhost/t...ganizacniJednotka
  • 21110
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