"Influence of Drainage on Landscape Functioning in \u0160umava National Park"@cs . "Braunschweig" . "drainage;remote sensing;Landsat"@en . "Tech. Univ. Braunschweig" . "Berchtesgaden" . . "12220" . "1"^^ . . "1"^^ . "Extended Abstract - International conference on Hydrology of Mountains Environments. Berchtesgaden, Federal Republic of Germany, 27 September - 1 october 2004." . "Influence of Drainage on Landscape Functioning in \u0160umava National Park" . "125" . . . "Influence of Drainage on Landscape Functioning in \u0160umava National Park"@cs . "Hais, Martin" . "RIV/60076658:12220/04:00005276" . . . "1"^^ . . . "RIV/60076658:12220/04:00005276!RIV/2005/MSM/122205/N" . "The research is engaged in the influence of drainage on the landscape functioning. The investigation is taking place in the central part of the National Park Sumava, in the cooperation with Administration (NP). For this project, three catchments in the upper \u0160umava area were chosen: 1. The Roklansk\u00FD and Modravsk\u00FD streams catchment (94 km2); 2. Kvildsk\u00FD stream and the upper part of Tepl\u00E1 Vltava (23 km2); 3. Hamersk\u00FD stream (21 km2).These catchments were chosen because the water balance of each could be measured. Also, there were large differences in the extent of drainage in each catchment. The first catchment, to a large extent, had been heavily disturbed by infestations of barkbeetle and die-back of trees. The network of drainage ditches were mapped in the field with the help of GPS. Fluctuations in the outflow will be evaluated from Czech Hydrometeorological Institute data. Local air and ground temperatures were measured using temperature data-loggers. Changes in the areal temperature distribution"@en . . . "Pro \u00FA\u010Dely t\u00E9to pr\u00E1ce byly zvoleny t\u0159i povod\u00ED nal\u00E9zaj\u00EDc\u00ED se v centr\u00E1ln\u00ED \u010D\u00E1sti \u0160umavy: povod\u00ED Roklansk\u00E9ho a Modravsk\u00E9ho potoka (94 km2) povod\u00ED povod\u00ED horn\u00EDho toku Tepl\u00E9 Vltavy k soutoku s Kvildsk\u00FDm potokem (23 km2), povod\u00ED Hamersk\u00E9ho potoka (21 km2). D\u016Fvodem volby pr\u00E1v\u011B t\u011Bchto povod\u00ED je mo\u017Enost vyu\u017Eit\u00ED hydrologick\u00E9 datov\u00E9 \u0159ady z \u010CHM\u00DA, rozd\u00EDln\u00E1 m\u00EDra k\u016Frovcov\u00E9 kalamity a p\u0159edpokl\u00E1dan\u00FD rozd\u00EDln\u00FD pod\u00EDl odvodn\u011Bn\u00FDch ploch.Pr\u00E1ce prezentuje p\u0159edb\u011B\u017En\u00E9 v\u00FDsledky s c\u00EDlem uk\u00E1zat metodick\u00E9 p\u0159\u00EDstupy, zejm\u00E9na d\u00E1lkov\u00E9ho pr\u016Fzkumu zem\u011B a p\u0159ibl\u00ED\u017Een\u00ED n\u011Bkter\u00FDch mo\u017En\u00FDch souvislost\u00ED t\u00FDkaj\u00EDc\u00EDch se odvodn\u011Bn\u00ED \u0160umavy.V sou\u010Dasn\u00E9 dob\u011B je zmapov\u00E1na podstatn\u00E1 \u010D\u00E1st meliora\u010Dn\u00EDch r\u00FDh a p\u0159evedena do prost\u0159ed\u00ED GIS. Na z\u00E1klad\u011B vektorov\u00FDch lini\u00ED budou d\u00E1le stanoveny polygony odvodn\u011Bn\u00FDch ploch a tato data budou d\u00E1le korelov\u00E1na s t\u0159\u00EDdami relativn\u00EDch teplot a vlhkost\u00ED krajinn\u00E9ho krytu a hodnotami jejich zm\u011Bn v \u010Dase. Podle prvn\u00EDch v\u00FDsledk\u016F mapov\u00E1n\u00ED lze usuzovat, \u017Ee k antropogenn\u00EDmu odvodn\u011Bn\u00ED do\u0161lo u p\u0159ev\u00E1\u017En\u00E9 v\u011Bt\u0161iny modravsk\u00FDch slat\u00ED"@cs . "[D327E113C224]" . "Influence of Drainage on Landscape Functioning in \u0160umava National Park" . "2004-01-01+01:00"^^ . "567856" . . "Z(MSM 122200003)" . . "Influence of Drainage on Landscape Functioning in \u0160umava National Park"@en . "Influence of Drainage on Landscape Functioning in \u0160umava National Park"@en . . . "The research is engaged in the influence of drainage on the landscape functioning. The investigation is taking place in the central part of the National Park Sumava, in the cooperation with Administration (NP). For this project, three catchments in the upper \u0160umava area were chosen: 1. The Roklansk\u00FD and Modravsk\u00FD streams catchment (94 km2); 2. Kvildsk\u00FD stream and the upper part of Tepl\u00E1 Vltava (23 km2); 3. Hamersk\u00FD stream (21 km2).These catchments were chosen because the water balance of each could be measured. Also, there were large differences in the extent of drainage in each catchment. The first catchment, to a large extent, had been heavily disturbed by infestations of barkbeetle and die-back of trees. The network of drainage ditches were mapped in the field with the help of GPS. Fluctuations in the outflow will be evaluated from Czech Hydrometeorological Institute data. Local air and ground temperatures were measured using temperature data-loggers. Changes in the areal temperature distribution" . . .