"33;41" . "580744" . "[D09A5EC7246D]" . "RIV/62156489:43210/04:00000715!RIV/2005/MSM/432105/N" . "Dufkov\u00E1, Jana" . . "9"^^ . . . "52" . "RIV/62156489:43210/04:00000715" . . "Wind erosion is caused by meteorological factors such as wind, precipitation and evaporation that influence the soil humidity. Erosive-climatological factor expresses wind and humidity conditions of particular landscape. This is an index of the influence of average soil surface humidity and average wind velocity on average soil erodibility by wind. On the basis of average wind velocity and Kon\u010Dek's humidity index, the values of the erosive-climatological factor for three chosen areas of Czech republic (Tel\u010D-Kosteln\u00ED Myslov\u00E1, Znojmo-Kucha\u0159ovice and Brno-Tu\u0159any), where the processes of wind erosion could exist, were evaluated. Thus, the change of the factor's value during the period of 1961 -- 2000 was studied. The linear trend for the region of Brno and Znojmo (dry areas) shows increasing threat of soils by wind erosion, the contrary situation is at the humid area (Tel\u010D). The results prove the influence of soil humidity on the erosive-climatological factor and hereby the influence on wind erosion sprea"@en . "Acta Universitatis Agriculturae et Silviculturae Mendelianae Brunensis" . "Potenci\u00E1ln\u00ED ohro\u017Eenost p\u016Fd ji\u017En\u00ED Moravy v\u011Btrnou eroz\u00ED" . "CZ - \u010Cesk\u00E1 republika" . . . . "Potential threat of southern Moravia soils by wind erosion"@en . "Kon\u010Dek's humidity index;erosive-climatological factor;wind erosion"@en . "1"^^ . . . "Potenci\u00E1ln\u00ED ohro\u017Eenost p\u016Fd ji\u017En\u00ED Moravy v\u011Btrnou eroz\u00ED"@cs . "1"^^ . . . "Potenci\u00E1ln\u00ED ohro\u017Eenost p\u016Fd ji\u017En\u00ED Moravy v\u011Btrnou eroz\u00ED" . "Z meteorologick\u00FDch faktor\u016F p\u016Fsob\u00EDc\u00EDch v\u011Btrnou erozi jsou to p\u0159edev\u0161\u00EDm pom\u011Bry v\u011Btrn\u00E9, sr\u00E1\u017Eky a v\u00FDpar ovliv\u0148uj\u00EDc\u00ED vlhkost p\u016Fdy. Erozn\u011B klimatick\u00FD faktor pak vyjad\u0159uje v\u011Btrn\u00E9 a vlhkostn\u00ED podm\u00EDnky dan\u00E9ho \u00FAzem\u00ED. Je to index vlivu pr\u016Fm\u011Brn\u00E9 vlhkosti p\u016Fdn\u00EDho povrchu a pr\u016Fm\u011Brn\u00E9 rychlosti v\u011Btru na pr\u016Fm\u011Brnou erodovatelnost p\u016Fdy v\u011Btrem. Na z\u00E1klad\u011B pr\u016Fm\u011Brn\u00E9 rychlosti v\u011Btru a Kon\u010Dekova indexu zavla\u017Een\u00ED byly vypo\u010Dteny hodnoty erozn\u011B klimatick\u00E9ho faktoru pro t\u0159i vybran\u00E9 oblasti \u010Cesk\u00E9 republiky (Tel\u010D-Kosteln\u00ED Myslov\u00E1, Znojmo-Kucha\u0159ovice a Brno-Tu\u0159any), v nich\u017E m\u016F\u017Ee doch\u00E1zet k proces\u016Fm v\u011Btrn\u00E9 eroze. Sledovala se tak p\u0159edev\u0161\u00EDm zm\u011Bna hodnot faktoru b\u011Bhem obdob\u00ED 1961 -- 2000. Line\u00E1rn\u00ED trend pro oblast Brna a Znojma, tedy oblasti such\u00E9, ukazuje na zvy\u0161uj\u00EDc\u00ED se stupe\u0148 ohro\u017Een\u00ED p\u016Fd v\u011Btrnou eroz\u00ED, u oblasti vlhk\u00E9 (Tel\u010D) je tomu pr\u00E1v\u011B naopak. V\u00FDsledky dokl\u00E1daj\u00ED vliv vlhkosti p\u016Fdy na erozn\u011B klimatick\u00FD faktor a t\u00EDm i na roz\u0161\u00ED\u0159en\u00ED v\u011Btrn\u00E9 eroze." . . "Potenci\u00E1ln\u00ED ohro\u017Eenost p\u016Fd ji\u017En\u00ED Moravy v\u011Btrnou eroz\u00ED"@cs . . "2" . "Z(MSM 432100001)" . "Potential threat of southern Moravia soils by wind erosion"@en . "43210" . . "Z meteorologick\u00FDch faktor\u016F p\u016Fsob\u00EDc\u00EDch v\u011Btrnou erozi jsou to p\u0159edev\u0161\u00EDm pom\u011Bry v\u011Btrn\u00E9, sr\u00E1\u017Eky a v\u00FDpar ovliv\u0148uj\u00EDc\u00ED vlhkost p\u016Fdy. Erozn\u011B klimatick\u00FD faktor pak vyjad\u0159uje v\u011Btrn\u00E9 a vlhkostn\u00ED podm\u00EDnky dan\u00E9ho \u00FAzem\u00ED. Je to index vlivu pr\u016Fm\u011Brn\u00E9 vlhkosti p\u016Fdn\u00EDho povrchu a pr\u016Fm\u011Brn\u00E9 rychlosti v\u011Btru na pr\u016Fm\u011Brnou erodovatelnost p\u016Fdy v\u011Btrem. Na z\u00E1klad\u011B pr\u016Fm\u011Brn\u00E9 rychlosti v\u011Btru a Kon\u010Dekova indexu zavla\u017Een\u00ED byly vypo\u010Dteny hodnoty erozn\u011B klimatick\u00E9ho faktoru pro t\u0159i vybran\u00E9 oblasti \u010Cesk\u00E9 republiky (Tel\u010D-Kosteln\u00ED Myslov\u00E1, Znojmo-Kucha\u0159ovice a Brno-Tu\u0159any), v nich\u017E m\u016F\u017Ee doch\u00E1zet k proces\u016Fm v\u011Btrn\u00E9 eroze. Sledovala se tak p\u0159edev\u0161\u00EDm zm\u011Bna hodnot faktoru b\u011Bhem obdob\u00ED 1961 -- 2000. Line\u00E1rn\u00ED trend pro oblast Brna a Znojma, tedy oblasti such\u00E9, ukazuje na zvy\u0161uj\u00EDc\u00ED se stupe\u0148 ohro\u017Een\u00ED p\u016Fd v\u011Btrnou eroz\u00ED, u oblasti vlhk\u00E9 (Tel\u010D) je tomu pr\u00E1v\u011B naopak. V\u00FDsledky dokl\u00E1daj\u00ED vliv vlhkosti p\u016Fdy na erozn\u011B klimatick\u00FD faktor a t\u00EDm i na roz\u0161\u00ED\u0159en\u00ED v\u011Btrn\u00E9 eroze."@cs . "1211-8516" . .