"RIV/00020711:_____/10:00003247" . . . "Spatial and temporal variability of hydrological drought under the climate change conditions over the Czech Republic"@en . "\u010Casov\u00E1 a plo\u0161n\u00E1 variabilita hydrologick\u00E9ho sucha v podm\u00EDnk\u00E1ch klimatick\u00E9 zm\u011Bny na \u00FAzem\u00ED \u010Cesk\u00E9 republiky" . "\u010Casov\u00E1 a plo\u0161n\u00E1 variabilita hydrologick\u00E9ho sucha v podm\u00EDnk\u00E1ch klimatick\u00E9 zm\u011Bny na \u00FAzem\u00ED \u010Cesk\u00E9 republiky" . "\u010Casov\u00E1 a plo\u0161n\u00E1 variabilita hydrologick\u00E9ho sucha v podm\u00EDnk\u00E1ch klimatick\u00E9 zm\u011Bny na \u00FAzem\u00ED \u010Cesk\u00E9 republiky"@cs . "[A0925BD8B8F8]" . "\u010Casov\u00E1 a plo\u0161n\u00E1 variabilita hydrologick\u00E9ho sucha v podm\u00EDnk\u00E1ch klimatick\u00E9 zm\u011Bny na \u00FAzem\u00ED \u010Cesk\u00E9 republiky"@cs . "Vizina, Adam" . . . . . "Metoda zn\u00E1m\u00E1 jako ,,threshold level%22 byla pou\u017Eita k anal\u00FDze \u010Dasov\u00FDch \u0159ad odtoku ve 118 vodo\u010Detn\u00FDch stanic\u00EDch v obdob\u00ED 1931\u20132007. V\u00FDstupem byly standardizovan\u00E9 nedostatkov\u00E9 objemy a jejich trv\u00E1n\u00ED pod limitem Q70 a Q95. Nejv\u00FDrazn\u011Bj\u0161\u00ED such\u00E9 epizody byly identifikov\u00E1ny v n\u00E1sleduj\u00EDc\u00EDch letech: 1947, 1953, 2003, 1992, a tak\u00E9 1950, 1983, 1990, 1962, 2004, 1951. Byly navr\u017Eeny kategorie sucha pod limitem Q95: m\u00EDrn\u00E9 (0,2\u20130,8), v\u00E1\u017En\u00E9 (0,8\u20131,5), velmi v\u00E1\u017En\u00E9 (1,5\u20132,5) a extr\u00E9mn\u00ED (>2,5). N\u00E1dr\u017Ee se pod\u00EDl\u00ED na zm\u00EDr\u0148ov\u00E1n\u00ED z\u00E1va\u017Enosti such\u00FDch epizod v p\u0159ev\u00E1\u017En\u00E9 v\u011Bt\u0161in\u011B p\u0159\u00EDpad\u016F. Simulace v\u00FDvoje klimatu podle sc\u00E9n\u00E1\u0159\u016F A1B, A2 a B2 uk\u00E1zala, \u017Ee lze o\u010Dek\u00E1vat zv\u00FD\u0161en\u00ED z\u00E1va\u017Enosti i frekvence sucha, a\u010Dkoli v sou\u010Dasn\u00FDch \u0159ad\u00E1ch byly nalezeny jak rostouc\u00ED tak i klesaj\u00EDc\u00ED trendy v\u00FDskytu sucha. Povod\u00ED s podlo\u017E\u00EDm budovan\u00FDm j\u00EDlovci vyk\u00E1zala statisticky v\u00FDznamn\u011B vy\u0161\u0161\u00ED tendenci k v\u00FDskytu sucha."@cs . . "Ka\u0161p\u00E1rek, Ladislav" . "P(SP/1A6/125/08)" . . . "RIV/00020711:_____/10:00003247!RIV12-MZP-00020711" . "Praha" . "Spatial and temporal variability of hydrological drought under the climate change conditions over the Czech Republic"@en . . "Neuvedena" . . "The threshold level approach was used to analyze discharge series of 118 gauging stations bellow Q70 and Q95 threshold in the period 1931\u20132007 with the standardized deficit volume and duration as drought parameters. The most distinct drought episodes were identified in following years sorted by severity: 1953, 1947, 2003, 1992, 1983, 1962, 1950, 1990, 1951 and adjacent years. The following categories of drought expressed below the Q95 threshold were suggested: moderate (0.2\u20130.8), serious (0.8\u20131.5), severe (1.5\u20132.5) and extreme (>2.5). The impact of reservoirs was found to reduce drought severity in overwhelming number of cases. The simulation using the climate development within A1B, A2 and B2 SRES scenario revealed that drought severity and frequency might be emphasized in the near future, though both increasing and decreasing trends can be found in present records. The basins built on mudstones showed significantly higher tendency to drought occurrence."@en . "Hansl\u00EDk, Eduard" . "V\u00FDzkumn\u00FD \u00FAstav vodohospod\u00E1\u0159sk\u00FD T.G.Masaryka, v.v.i." . . . . "\u0160imek, Pavel" . "5"^^ . "hydrological drought; threshold level; deficit volume; drought duration; climate change; water quality"@en . "150"^^ . . "\u010Casov\u00E1 a plo\u0161n\u00E1 variabilita hydrologick\u00E9ho sucha v podm\u00EDnk\u00E1ch klimatick\u00E9 zm\u011Bny na \u00FAzem\u00ED \u010Cesk\u00E9 republiky" . . . . "Metoda zn\u00E1m\u00E1 jako ,,threshold level%22 byla pou\u017Eita k anal\u00FDze \u010Dasov\u00FDch \u0159ad odtoku ve 118 vodo\u010Detn\u00FDch stanic\u00EDch v obdob\u00ED 1931\u20132007. V\u00FDstupem byly standardizovan\u00E9 nedostatkov\u00E9 objemy a jejich trv\u00E1n\u00ED pod limitem Q70 a Q95. Nejv\u00FDrazn\u011Bj\u0161\u00ED such\u00E9 epizody byly identifikov\u00E1ny v n\u00E1sleduj\u00EDc\u00EDch letech: 1947, 1953, 2003, 1992, a tak\u00E9 1950, 1983, 1990, 1962, 2004, 1951. Byly navr\u017Eeny kategorie sucha pod limitem Q95: m\u00EDrn\u00E9 (0,2\u20130,8), v\u00E1\u017En\u00E9 (0,8\u20131,5), velmi v\u00E1\u017En\u00E9 (1,5\u20132,5) a extr\u00E9mn\u00ED (>2,5). N\u00E1dr\u017Ee se pod\u00EDl\u00ED na zm\u00EDr\u0148ov\u00E1n\u00ED z\u00E1va\u017Enosti such\u00FDch epizod v p\u0159ev\u00E1\u017En\u00E9 v\u011Bt\u0161in\u011B p\u0159\u00EDpad\u016F. Simulace v\u00FDvoje klimatu podle sc\u00E9n\u00E1\u0159\u016F A1B, A2 a B2 uk\u00E1zala, \u017Ee lze o\u010Dek\u00E1vat zv\u00FD\u0161en\u00ED z\u00E1va\u017Enosti i frekvence sucha, a\u010Dkoli v sou\u010Dasn\u00FDch \u0159ad\u00E1ch byly nalezeny jak rostouc\u00ED tak i klesaj\u00EDc\u00ED trendy v\u00FDskytu sucha. Povod\u00ED s podlo\u017E\u00EDm budovan\u00FDm j\u00EDlovci vyk\u00E1zala statisticky v\u00FDznamn\u011B vy\u0161\u0161\u00ED tendenci k v\u00FDskytu sucha." . "5"^^ . "249707" . . "978-80-87402-11-5" . "Vlnas, Radek" . . . "150"^^ . .