"The climate change scenarios for the Czech Republic (CR) are deduced from the Global Circulation Model simulations. Consequences of climate change will display differently in individual regions of the CR in dependence on natural conditions. Simulations of changes in hydrological regime proved that the average discharges of rivers in the CR would significantly decrease owing to the presumed climatic trend. Minimum discharges would radically decrease in most basins. This fact would cause serious problems in reservoirs with insufficient active storage capacity. Reduction of baseflow would be similar to reduction of total runoff. Basins in the southern part of the CR are more sensitive to climate change delimited by the applied scenarios than highland basins in the north part of the CR. Under the given climate scenarios flood frequency and magnitude is not increasing, but seasonal distribution changes. Floods occur more frequently in winter and less in spring."@en . "Ka\u0161p\u00E1rek, Ladislav" . "RIV/00020711:_____/05:00000770!RIV06-MZP-00020711" . "Hydrologick\u00E9 dni 2005" . "Region\u00E1ln\u00ED dopady klimatick\u00E9 zm\u011Bny na hydrologick\u00FD re\u017Eim v \u010CR"@cs . "Sc\u00E9n\u00E1\u0159e klimatick\u00E9 zm\u011Bny pro \u010Ceskou republiku jsou odvozeny ze simulac\u00ED model\u016F glob\u00E1ln\u00ED cirkulace atmosf\u00E9ry. D\u016Fsledky klimatick\u00E9 zm\u011Bny se v jednotliv\u00FDch regionech \u010CR projev\u00ED na hydrologick\u00E9m re\u017Eimu r\u016Fzn\u011B v z\u00E1vislosti na p\u0159\u00EDrodn\u00EDch podm\u00EDnk\u00E1ch povod\u00ED. Simulace zm\u011Bn hydrologick\u00E9ho re\u017Eimu uk\u00E1zaly, \u017Ee na \u00FAzem\u00ED \u010CR by p\u0159i p\u0159edpokl\u00E1dan\u00E9m v\u00FDvoji klimatu do\u0161lo k v\u00FDznamn\u00E9mu zmen\u0161en\u00ED pr\u016Fm\u011Brn\u00FDch pr\u016Ftok\u016F. Minim\u00E1ln\u00ED pr\u016Ftoky by se na v\u011Bt\u0161in\u011B povod\u00ED zmen\u0161ily velmi radik\u00E1ln\u011B. To by se projevilo v\u00E1\u017En\u00FDmi dopady na z\u00E1sobn\u00ED funkci n\u00E1dr\u017E\u00ED. Zmen\u0161en\u00ED podzemn\u00EDho odtoku by bylo obdobn\u00E9 jako u celkov\u00E9ho odtoku. Povod\u00ED na jihu a jihov\u00FDchod\u011B \u010CR jsou na zm\u011Bny klimatu popsan\u00E9 pou\u017Eit\u00FDmi sc\u00E9n\u00E1\u0159i citliv\u011Bj\u0161\u00ED ne\u017E povod\u00ED na ostatn\u00EDm \u00FAzem\u00ED, nejm\u00E9n\u011B jsou citliv\u00E1 horsk\u00E1 povod\u00ED v severn\u00ED \u010D\u00E1sti\u00FAzem\u00ED \u010CR. Pou\u017Eit\u00ED dan\u00FDch klimatick\u00FDch sc\u00E9n\u00E1\u0159\u016F neindikuje zv\u011Bt\u0161en\u00ED \u010Detnosti ani velikosti povodn\u00ED, m\u011Bn\u00ED se jejich sez\u00F3nn\u00ED chod. P\u0159ib\u00FDv\u00E1 zimn\u00EDch povod\u00ED, zmen\u0161uj\u00ED se povodn\u011B jarn\u00ED." . "3"^^ . . "climate change scenario; water balance; potential evapotranspiration; basin evaporation; total runoff; baseflow"@en . "2005-09-21+02:00"^^ . "RIV/00020711:_____/05:00000770" . . "Bratislava" . "3"^^ . "Bratislava" . "540490" . . . . . . . "Kr\u00E1tk\u00E1, Martina" . . . . "Region\u00E1ln\u00ED dopady klimatick\u00E9 zm\u011Bny na hydrologick\u00FD re\u017Eim v \u010CR" . "Z(MZP0002071101)" . . . "[7BE8F3410A5B]" . "The Regional Impacts of Climate Change on Hydrological Regime of the Czech Republic"@en . "Region\u00E1ln\u00ED dopady klimatick\u00E9 zm\u011Bny na hydrologick\u00FD re\u017Eim v \u010CR"@cs . . . . . "Region\u00E1ln\u00ED dopady klimatick\u00E9 zm\u011Bny na hydrologick\u00FD re\u017Eim v \u010CR" . . "80-88907-53-5" . . "Ministerstvo \u017Eivotn\u00EDho prost\u0159ed\u00ED \u010CR" . "6"^^ . "The Regional Impacts of Climate Change on Hydrological Regime of the Czech Republic"@en . . "389;394" . "Sc\u00E9n\u00E1\u0159e klimatick\u00E9 zm\u011Bny pro \u010Ceskou republiku jsou odvozeny ze simulac\u00ED model\u016F glob\u00E1ln\u00ED cirkulace atmosf\u00E9ry. D\u016Fsledky klimatick\u00E9 zm\u011Bny se v jednotliv\u00FDch regionech \u010CR projev\u00ED na hydrologick\u00E9m re\u017Eimu r\u016Fzn\u011B v z\u00E1vislosti na p\u0159\u00EDrodn\u00EDch podm\u00EDnk\u00E1ch povod\u00ED. Simulace zm\u011Bn hydrologick\u00E9ho re\u017Eimu uk\u00E1zaly, \u017Ee na \u00FAzem\u00ED \u010CR by p\u0159i p\u0159edpokl\u00E1dan\u00E9m v\u00FDvoji klimatu do\u0161lo k v\u00FDznamn\u00E9mu zmen\u0161en\u00ED pr\u016Fm\u011Brn\u00FDch pr\u016Ftok\u016F. Minim\u00E1ln\u00ED pr\u016Ftoky by se na v\u011Bt\u0161in\u011B povod\u00ED zmen\u0161ily velmi radik\u00E1ln\u011B. To by se projevilo v\u00E1\u017En\u00FDmi dopady na z\u00E1sobn\u00ED funkci n\u00E1dr\u017E\u00ED. Zmen\u0161en\u00ED podzemn\u00EDho odtoku by bylo obdobn\u00E9 jako u celkov\u00E9ho odtoku. Povod\u00ED na jihu a jihov\u00FDchod\u011B \u010CR jsou na zm\u011Bny klimatu popsan\u00E9 pou\u017Eit\u00FDmi sc\u00E9n\u00E1\u0159i citliv\u011Bj\u0161\u00ED ne\u017E povod\u00ED na ostatn\u00EDm \u00FAzem\u00ED, nejm\u00E9n\u011B jsou citliv\u00E1 horsk\u00E1 povod\u00ED v severn\u00ED \u010D\u00E1sti\u00FAzem\u00ED \u010CR. Pou\u017Eit\u00ED dan\u00FDch klimatick\u00FDch sc\u00E9n\u00E1\u0159\u016F neindikuje zv\u011Bt\u0161en\u00ED \u010Detnosti ani velikosti povodn\u00ED, m\u011Bn\u00ED se jejich sez\u00F3nn\u00ED chod. P\u0159ib\u00FDv\u00E1 zimn\u00EDch povod\u00ED, zmen\u0161uj\u00ED se povodn\u011B jarn\u00ED."@cs .