National Repository of Grey Literature 2 records found  Search took 0.01 seconds. 
Influence of precipitation and temperature in the period 1961–2100 on the possibilities to grow Picea abies in the Czech Republic
Cudlín, Pavel ; Štěpánek, P. ; Macků, J. ; Kohout, M. ; Rožnovský, J.
For environmental risk estimation of Norway spruce ecosystems under climate change, the space means for each „forest vegetation degree“ in the frame of all so called „natural forest areas“ basic climatic characteristics (above all mean daily diameter, daily precipitation sum) and two climatic extremes (number of days with daily precipitation sum < 1 mm, number of days with maximum temperature > 30 oC) were computed. Aggregate typological units, as“forest type sets” and “management types” in combination with “forest stand types”, were used for environmental risk estimation at „natural forest areas“ and whole Czech Republic levels. Endangered forest stands, occurred in given “forest type set”, „forest vegetation degree“ and „natural forest area“ were estimated using comparison of basic and derived climatic parameters between all 5 time period (1961–2099). Measured data from climatic stations were used for the period A (1961–1990) and B (1991–2009); for periods C (2010–2039), D (2040–2069) and E (2070–2099) the data were modeled by climatic model ALADIN-Climate/CZ. This procedure enabled to distinguish all „natural forest areas“ into “warm” ones, which do not meet requirements for ecological conditions of Norway spruce at present period B and “cold” ones which meet them
The temperature and precipitation course in Prague-Karlov, 1961-2010
Střeštík, Jaroslav
The course of temperatures and precipitation in Prague over the last 50 years is presented and compared with scenarios of the further development of the climate. The temperature increased significantly and this increase is more rapid than that of the global temperature. Precipitation totals display only very small decrease over the last 50 years. However, precipitation totals in spring decreased more than the annual sums and a remarkable decrease of days with heavy rainfall takes place. These facts contribute to the observed decrease of the amount of moisture in nature and to the increased occurrence of droughts. There is no indication that all these observed trends could be different in future.

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