About: Modeling of soil water content and soil temperature at selected U.S. and central European stations using SoilClim model     Goto   Sponge   NotDistinct   Permalink

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Description
  • Within the presented study the SoilClim model was tested through various climatic and soil conditions. SoilClim model enables to estimate reference and actual evapotranspiration from defined vegetation cover and consequently the soil water content within two defined layers (named as Moisture control section I and II) could be deduced. The soil temperature in 0.5 m depth is also estimated (on the basis of simple empirical model). Mentioned outputs could be additionally used for identification of soil climate regimes (both Hydric and Thermic) within selected location. The SoilClim works in daily step and needs daily maximum and minimum air temperature, global radiation, precipitation, air humidity and wind speed as input. The brief information about soil layers (field capacity, wilting point, depth) and vegetation cover is necessary. The algorithm for reference evapotranspiration is based on Penman-Monteith method.
  • Within the presented study the SoilClim model was tested through various climatic and soil conditions. SoilClim model enables to estimate reference and actual evapotranspiration from defined vegetation cover and consequently the soil water content within two defined layers (named as Moisture control section I and II) could be deduced. The soil temperature in 0.5 m depth is also estimated (on the basis of simple empirical model). Mentioned outputs could be additionally used for identification of soil climate regimes (both Hydric and Thermic) within selected location. The SoilClim works in daily step and needs daily maximum and minimum air temperature, global radiation, precipitation, air humidity and wind speed as input. The brief information about soil layers (field capacity, wilting point, depth) and vegetation cover is necessary. The algorithm for reference evapotranspiration is based on Penman-Monteith method. (en)
Title
  • Modeling of soil water content and soil temperature at selected U.S. and central European stations using SoilClim model
  • Modeling of soil water content and soil temperature at selected U.S. and central European stations using SoilClim model (en)
skos:prefLabel
  • Modeling of soil water content and soil temperature at selected U.S. and central European stations using SoilClim model
  • Modeling of soil water content and soil temperature at selected U.S. and central European stations using SoilClim model (en)
skos:notation
  • RIV/62156489:43210/09:00139780!RIV10-MSM-43210___
http://linked.open...avai/riv/aktivita
http://linked.open...avai/riv/aktivity
  • P(GP521/09/P479), P(ME 844), Z(MSM6215648905)
http://linked.open...iv/cisloPeriodika
  • 1
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
  • 326782
http://linked.open...ai/riv/idVysledku
  • RIV/62156489:43210/09:00139780
http://linked.open...riv/jazykVysledku
http://linked.open.../riv/klicovaSlova
  • temperature; water content; SoilClim (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...odStatuVydavatele
  • AT - Rakouská republika
http://linked.open...ontrolniKodProRIV
  • [8A6E82A73EA8]
http://linked.open...i/riv/nazevZdroje
  • European Geosciences Union, Vienna, 20 - 24 April 2009
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
  • 11
http://linked.open...iv/tvurceVysledku
  • Eitzinger, Josef
  • Hlavinka, Petr
  • Trnka, Miroslav
  • Žalud, Zdeněk
  • Balek, Jan
  • Hayes, Michael
  • Svoboda, Mark
http://linked.open...n/vavai/riv/zamer
issn
  • 1029-7006
number of pages
http://localhost/t...ganizacniJednotka
  • 43210
is http://linked.open...avai/riv/vysledek of
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