About: Runoff formation in a small catchment at hillslope and catchment scales     Goto   Sponge   NotDistinct   Permalink

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Description
  • The study is focused on runoff formation processes at two scales: the scale of a small mountainous catchment at its outlet and the scale of an experimental plot located in a typical hillslope subregion. The heterogeneous soil profile of the catchments is formed by Cambisols developed on granite bedrocks. The surface runoff appears rarely, the subsurface flow forms a dominant part of the hydrograph. The dynamic thresholds of rainfall totals apparently control the ratio and the magnitude of stormflow at both scales. Up to the threshold value, the runoff strongly depends on the initial saturation conditions. Above the threshold value, the initial soil moisture conditions are less important.
  • The study is focused on runoff formation processes at two scales: the scale of a small mountainous catchment at its outlet and the scale of an experimental plot located in a typical hillslope subregion. The heterogeneous soil profile of the catchments is formed by Cambisols developed on granite bedrocks. The surface runoff appears rarely, the subsurface flow forms a dominant part of the hydrograph. The dynamic thresholds of rainfall totals apparently control the ratio and the magnitude of stormflow at both scales. Up to the threshold value, the runoff strongly depends on the initial saturation conditions. Above the threshold value, the initial soil moisture conditions are less important. (en)
Title
  • Runoff formation in a small catchment at hillslope and catchment scales
  • Runoff formation in a small catchment at hillslope and catchment scales (en)
skos:prefLabel
  • Runoff formation in a small catchment at hillslope and catchment scales
  • Runoff formation in a small catchment at hillslope and catchment scales (en)
skos:notation
  • RIV/68407700:21110/10:00168080!RIV11-MZP-21110___
http://linked.open...avai/riv/aktivita
http://linked.open...avai/riv/aktivity
  • P(GA205/09/0831), P(SP/2E7/229/07), Z(MSM6840770002), Z(MZP0002071101)
http://linked.open...iv/cisloPeriodika
  • 16
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
  • 286137
http://linked.open...ai/riv/idVysledku
  • RIV/68407700:21110/10:00168080
http://linked.open...riv/jazykVysledku
http://linked.open.../riv/klicovaSlova
  • catchment; hillslope; rainfall-runoff episodes; soil moisture; subsurface trench (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...odStatuVydavatele
  • US - Spojené státy americké
http://linked.open...ontrolniKodProRIV
  • [24040E44DF62]
http://linked.open...i/riv/nazevZdroje
  • Hydrological Processes
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...v/svazekPeriodika
  • 24
http://linked.open...iv/tvurceVysledku
  • Císlerová, Milena
  • Šanda, Martin
  • Hrnčíř, Miroslav
  • Kulasová, A.
http://linked.open...ain/vavai/riv/wos
  • 000280142100005
http://linked.open...n/vavai/riv/zamer
issn
  • 0885-6087
number of pages
http://localhost/t...ganizacniJednotka
  • 21110
is http://linked.open...avai/riv/vysledek of
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