"BILAN water balance model in daily time step"@en . "Z(MZP0002071101)" . "326662" . "V\u00DAV T.G.M. v.v.i Odd\u011Blen\u00ED 211" . "Byl vyvinut model umo\u017E\u0148uj\u00EDc\u00ED vyhodnocen\u00ED komponent hydrologick\u00E9 bilance povod\u00ED v denn\u00EDm \u010Dasov\u00E9m kroku. Struktura modelu je tvo\u0159ena syst\u00E9mem vztah\u016F zohled\u0148uj\u00EDc\u00EDch z\u00E1kladn\u00ED fyzik\u00E1ln\u00ED principy hydrologick\u00FDch proces\u016F prob\u00EDhaj\u00EDc\u00EDch na povrchu p\u016Fdy, v z\u00F3n\u011B aerace (v\u010Detn\u011B zahrnut\u00ED vlivu vegeta\u010Dn\u00EDho pokryvu) a v podzemn\u00ED vod\u011B. Teplota vzduchu slou\u017E\u00ED jako indik\u00E1tor energetick\u00FDch podm\u00EDnek v\u00FDznamn\u011B ovliv\u0148uj\u00EDc\u00EDch prvky hydrologick\u00E9 bilance. Vstupem do modelu jsou denn\u00ED \u010Dasov\u00E9 \u0159ady sr\u00E1\u017Eek, teploty vzduchu a relativn\u00ED vlhkosti vzduchu. Kalibrace parametr\u016F modelu prob\u00EDh\u00E1 na pozorovan\u00FDch \u010Dasov\u00FDch \u0159ad\u00E1ch pr\u016Ftoku. Model generuje denn\u00ED \u010Dasov\u00E9 \u0159ady potenci\u00E1ln\u00ED evapotranspirace, \u00FAzemn\u00EDho v\u00FDparu, z\u00E1soby vody ve sn\u011Bhov\u00E9m pokryvu, v z\u00F3n\u011B aerace, z\u00E1sobu podzemn\u00ED vody a mno\u017Estv\u00ED vody dostupn\u00E9 pro p\u0159\u00EDm\u00FD odtok. Celkov\u00FD odtok se skl\u00E1d\u00E1 ze dvou slo\u017Eek: p\u0159\u00EDm\u00E9ho a z\u00E1kladn\u00EDho odtoku. Model BILAN v denn\u00EDm kroku m\u00E1 \u0161est parametr\u016F, jejich\u017E hodnoty jsou odhadnuty pomoc\u00ED optimaliza\u010Dn\u00EDho algoritmu." . "Model hydrologick\u00E9 bilance BILAN v denn\u00EDm \u010Dasov\u00E9m kroku"@cs . "Mathematical modelling; hydrological balance; runoff; precipitation; air temperature; relative humidity"@en . "Model hydrologick\u00E9 bilance BILAN v denn\u00EDm \u010Dasov\u00E9m kroku" . . "Hanel, Martin" . . . "BILAN water balance model in daily time step"@en . . "Model hydrologick\u00E9 bilance BILAN v denn\u00EDm \u010Dasov\u00E9m kroku"@cs . . . "[86A536CB9F9A]" . . "RIV/00020711:_____/09:00002714" . . . . "Model hydrologick\u00E9 bilance BILAN v denn\u00EDm \u010Dasov\u00E9m kroku" . "Ka\u0161p\u00E1rek, Ladislav" . . "Hor\u00E1\u010Dek, Stanislav" . "RIV/00020711:_____/09:00002714!RIV10-MZP-00020711" . . "Byl vyvinut model umo\u017E\u0148uj\u00EDc\u00ED vyhodnocen\u00ED komponent hydrologick\u00E9 bilance povod\u00ED v denn\u00EDm \u010Dasov\u00E9m kroku. Struktura modelu je tvo\u0159ena syst\u00E9mem vztah\u016F zohled\u0148uj\u00EDc\u00EDch z\u00E1kladn\u00ED fyzik\u00E1ln\u00ED principy hydrologick\u00FDch proces\u016F prob\u00EDhaj\u00EDc\u00EDch na povrchu p\u016Fdy, v z\u00F3n\u011B aerace (v\u010Detn\u011B zahrnut\u00ED vlivu vegeta\u010Dn\u00EDho pokryvu) a v podzemn\u00ED vod\u011B. Teplota vzduchu slou\u017E\u00ED jako indik\u00E1tor energetick\u00FDch podm\u00EDnek v\u00FDznamn\u011B ovliv\u0148uj\u00EDc\u00EDch prvky hydrologick\u00E9 bilance. Vstupem do modelu jsou denn\u00ED \u010Dasov\u00E9 \u0159ady sr\u00E1\u017Eek, teploty vzduchu a relativn\u00ED vlhkosti vzduchu. Kalibrace parametr\u016F modelu prob\u00EDh\u00E1 na pozorovan\u00FDch \u010Dasov\u00FDch \u0159ad\u00E1ch pr\u016Ftoku. Model generuje denn\u00ED \u010Dasov\u00E9 \u0159ady potenci\u00E1ln\u00ED evapotranspirace, \u00FAzemn\u00EDho v\u00FDparu, z\u00E1soby vody ve sn\u011Bhov\u00E9m pokryvu, v z\u00F3n\u011B aerace, z\u00E1sobu podzemn\u00ED vody a mno\u017Estv\u00ED vody dostupn\u00E9 pro p\u0159\u00EDm\u00FD odtok. Celkov\u00FD odtok se skl\u00E1d\u00E1 ze dvou slo\u017Eek: p\u0159\u00EDm\u00E9ho a z\u00E1kladn\u00EDho odtoku. Model BILAN v denn\u00EDm kroku m\u00E1 \u0161est parametr\u016F, jejich\u017E hodnoty jsou odhadnuty pomoc\u00ED optimaliza\u010Dn\u00EDho algoritmu."@cs . . "Bilan denn\u00ED verze" . . . . . . . . "3"^^ . "3"^^ . "Program prost\u0159ed\u00ED DELPHI (Pascal)" . . . "This model has been developed for assessing water balance components of a catchment in a daily time step. The structure of the model is formed by a system of relationships describing basic principles of water balance on soil surface, in the zone of aeration, including the effect of vegetation cover, and in groundwater zone. Air temperature is used as an indicator of energy conditions, which affect significantly the water balance components. The entry data of the model are daily series of basin precipitation, the air temperature and relative air humidity. In calibrating parameters of the model, daily runoff series at the outlet from the basin are used. The model generates daily series of basin potential evapotranspiration, actual evaporation, water storage components in the snow cover, zone of aeration (soil), direct runoff storage and groundwater aquifer. The total runoff consists of two components, which are direct runoff and base flow."@en .