"Pro hodnocen\u00ED v\u00FDvoje klimatick\u00FDch faktor\u016F v\u00FDskytu v\u011Btrn\u00E9 eroze v jarn\u00EDm obdob\u00ED (b\u0159ezen a duben) byla pou\u017Eita data o stavu povrchu hol\u00E9 p\u016Fdy z 29 stanic s\u00EDt\u011B \u010Cesk\u00E9ho hydrometeorologick\u00E9ho \u00FAstavu. Po\u010Det dn\u016F se such\u00FDm povrchem p\u016Fdy v ka\u017Ed\u00E9m roce byl srovn\u00E1n s pr\u016Fm\u011Brn\u00FDm po\u010Dtem such\u00FDch dn\u016F v obdob\u00ED 1961--2010. Byla zji\u0161t\u011Bna pr\u016Fkazn\u00E1 z\u00E1vislost (p<0,01) mezi po\u010Dtem dn\u016F se such\u00FDm povrchem p\u016Fdy a nadmo\u0159skou v\u00FD\u0161kou (r = -0,51, n = 29). Anal\u00FDza trendu \u010Dasov\u00E9 \u0159ady nevykazuje jednozna\u010Dn\u00FD trend r\u016Fstu \u010Di poklesu v\u00FDskytu such\u00FDch obdob\u00ED. Nicm\u00E9n\u011B, v posledn\u00ED kompletn\u00ED dek\u00E1d\u011B (2001 -- 2010) byly \u010Dty\u0159i roky (2002, 2003, 2007 a 2009) klasifikov\u00E1ny jako such\u00E9 a dva (2001 a 2006) jako vlhk\u00E9. To nasv\u011Bd\u010Duje r\u016Fstu extremity po\u010Das\u00ED v jarn\u00EDm obdob\u00ED." . . "4"^^ . "P(QJ1220054)" . "Dlouhodob\u00FD v\u00FDvoj klimatick\u00FDch faktor\u016F v\u00FDskytu v\u011Btrn\u00E9 eroze" . "0139-6013" . "RIV/62156489:43210/13:00209781" . . "CZ - \u010Cesk\u00E1 republika" . "Long term development of wind erosion climatic factors"@en . "Long term development of wind erosion climatic factors"@en . . "12" . "St\u0159eda, Tom\u00E1\u0161" . "http://www.vupt.cz/content/files/aktualni_poznatky/vedecka_priloha_2013.pdf" . . . . . "Dlouhodob\u00FD v\u00FDvoj klimatick\u00FDch faktor\u016F v\u00FDskytu v\u011Btrn\u00E9 eroze"@cs . "43210" . "70122" . "wind erosion; soil moisture; soil surface"@en . . . "Dlouhodob\u00FD v\u00FDvoj klimatick\u00FDch faktor\u016F v\u00FDskytu v\u011Btrn\u00E9 eroze" . "To evaluate moisture conditions in spring period, data of bare soil surface state were used. Analysis included 29 stations throughout the Czech Republic. Number of days with dry soil surface in each year was compared with the average number of those days in the period 1961--2010 for a given station. There is a significant correlation (p<0.01) between number of days with dry condition of soil and elevation (r = -0.51, n = 29). Trend analysis did not produce conclusive results, but linear trend of smoothing April data was significantly increased in most localities. The number of days with dry condition of soil in the past decades has no significant upward or downward trend. However in recent years four years (2002, 2003, 2007 and 2009) have been evaluated as dry and two (2001 and 2006) as wet. An amount of extreme spring weather increases."@en . . . "3"^^ . . "[727AAD4C4E16]" . . "St\u0159edov\u00E1, Hana" . "\u00DAroda" . "Pro hodnocen\u00ED v\u00FDvoje klimatick\u00FDch faktor\u016F v\u00FDskytu v\u011Btrn\u00E9 eroze v jarn\u00EDm obdob\u00ED (b\u0159ezen a duben) byla pou\u017Eita data o stavu povrchu hol\u00E9 p\u016Fdy z 29 stanic s\u00EDt\u011B \u010Cesk\u00E9ho hydrometeorologick\u00E9ho \u00FAstavu. Po\u010Det dn\u016F se such\u00FDm povrchem p\u016Fdy v ka\u017Ed\u00E9m roce byl srovn\u00E1n s pr\u016Fm\u011Brn\u00FDm po\u010Dtem such\u00FDch dn\u016F v obdob\u00ED 1961--2010. Byla zji\u0161t\u011Bna pr\u016Fkazn\u00E1 z\u00E1vislost (p<0,01) mezi po\u010Dtem dn\u016F se such\u00FDm povrchem p\u016Fdy a nadmo\u0159skou v\u00FD\u0161kou (r = -0,51, n = 29). Anal\u00FDza trendu \u010Dasov\u00E9 \u0159ady nevykazuje jednozna\u010Dn\u00FD trend r\u016Fstu \u010Di poklesu v\u00FDskytu such\u00FDch obdob\u00ED. Nicm\u00E9n\u011B, v posledn\u00ED kompletn\u00ED dek\u00E1d\u011B (2001 -- 2010) byly \u010Dty\u0159i roky (2002, 2003, 2007 a 2009) klasifikov\u00E1ny jako such\u00E9 a dva (2001 a 2006) jako vlhk\u00E9. To nasv\u011Bd\u010Duje r\u016Fstu extremity po\u010Das\u00ED v jarn\u00EDm obdob\u00ED."@cs . "Mu\u017E\u00EDkov\u00E1, Bronislava" . "RIV/62156489:43210/13:00209781!RIV14-MZE-43210___" . "3"^^ . . . . . . "Dlouhodob\u00FD v\u00FDvoj klimatick\u00FDch faktor\u016F v\u00FDskytu v\u011Btrn\u00E9 eroze"@cs .