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National Repository of Grey Literature 2 records found  Search took 0.01 seconds. 
Snow cover at the Čertova louka and the Modré sedlo sites (Krkonoše Mts) in winter 2010/2011
 Tryzna, Vojtěch ; Engel, Zbyněk (advisor) ; Nyplová, Petra (referee)
Snow cover at the studied locations in the Eastern Giant Mountains in the winter of 2010/2011 were collected through periodic field measurements of snow cover height. For evaluation and interpretation of measurements was used data from the meteorological station on "Luční bouda" and published the results of previous measurements in the field. In the "Čertova louka" is located nivation hollow, which show an increase in the accumulation of snow, which melted in early June. In the "Modré sedlo" location, which is largely exposed to deflation, the snow lasted until the end of April. The distribution of snow cover at both sites in winter 2010/2011 were consistent with previous observations. Maximum height of snow cover was lowest (about 8.4 to 43.8 %) from the current observation and were recorded aproximately one month earlier (18. 2.). The main reason for the development of unusual snow was warm front with rainfall, which affected the studied area during March. Winter 2010/2011 has been in terms of power and duration of snow cover at the studied locations below average.
Detailed record
Snow cover at the Čertova louka and the Modré sedlo sites (Krkonoše Mts) in winter 2010/2011
 Tryzna, Vojtěch ; Engel, Zbyněk (advisor) ; Nyplová, Petra (referee)
Snow cover at the studied locations in the Eastern Giant Mountains in the winter of 2010/2011 were collected through periodic field measurements of snow cover height. For evaluation and interpretation of measurements was used data from the meteorological station on "Luční bouda" and published the results of previous measurements in the field. In the "Čertova louka" is located nivation hollow, which show an increase in the accumulation of snow, which melted in early June. In the "Modré sedlo" location, which is largely exposed to deflation, the snow lasted until the end of April. The distribution of snow cover at both sites in winter 2010/2011 were consistent with previous observations. Maximum height of snow cover was lowest (about 8.4 to 43.8 %) from the current observation and were recorded aproximately one month earlier (18. 2.). The main reason for the development of unusual snow was warm front with rainfall, which affected the studied area during March. Winter 2010/2011 has been in terms of power and duration of snow cover at the studied locations below average.
Detailed record

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