DOBROVOLNÝ, Petr and Rudolf BRÁZDIL. Long-term trends in strong winds in the Czech Republic. In Geophysical Research Abstracts, EGU General Assembly, Vol. 8. Vienna: European Geophysical Union, 2006, p. 1. ISSN 1607-7962.
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Basic information
Original name Long-term trends in strong winds in the Czech Republic
Name in Czech Dolohodobé trendy ve výsyktu silných větrů v České republice
Authors DOBROVOLNÝ, Petr (203 Czech Republic, guarantor) and Rudolf BRÁZDIL (203 Czech Republic).
Edition Vienna, Geophysical Research Abstracts, EGU General Assembly, Vol. 8, p. 1-1, 2006.
Publisher European Geophysical Union
Other information
Original language English
Type of outcome Proceedings paper
Field of Study 10500 1.5. Earth and related environmental sciences
Country of publisher Austria
Confidentiality degree is not subject to a state or trade secret
RIV identification code RIV/00216224:14310/06:00029016
Organization unit Faculty of Science
ISSN 1607-7962
Keywords in English strong winds; instrumental measurements; documentary evidence; long term trends; Czech Republic
Tags Czech Republic, documentary evidence, instrumental measurements, long term trends, strong winds
Tags International impact
Changed by Changed by: prof. RNDr. Petr Dobrovolný, CSc., učo 680. Changed: 9/4/2010 11:27.
Abstract
Wind measurements (speeds and gusts) on meteorological stations are biased by different factors complicating to develop homogeneous long-term series. Statistical analysis of wind gusts in 1961 to 1990 is presented. Strong winds are divided on windstorms related to large horizontal pressure gradients and strong winds connected with convection (squall, tornado, downburst). Using PCA of mean sea level pressure field types of winter windstorms are analysed for the 20th century. Long term series of strong winds from the 16th century are produced using information from documentary evidence (narrative sources, visual daily weather observations, newspapers etc.). Trends in strong winds are analysed with respect to circulation characteristics (NAOI, CEZI) and winter temperatures in Central Europe. Climatology of tornadoes is presented with respect to their seasonality, spatial distribution, impacts and intensity according to Fujita scale. Higher frequency of strong winds appears in the late 16th and in the early 17th centuries. It corresponds with the common deterioration of the Central European climate. On the other hand, the lower number of recorded events during the 1940s and 1950s is connected with the quality of data excerpted mostly from newspapers for this period. Documentary evidence allows identify the most disastrous historical windstorms and provides valuable information on impacts to nature and society. In such a way information of historical climatology complement data from the instrumental period and help to define the role of anthropogenic factor in present global climate change.
Abstract (in Czech)
Wind measurements (speeds and gusts) on meteorological stations are biased by different factors complicating to develop homogeneous long-term series. Statistical analysis of wind gusts in 1961 to 1990 is presented. Strong winds are divided on windstorms related to large horizontal pressure gradients and strong winds connected with convection (squall, tornado, downburst). Using PCA of mean sea level pressure field types of winter windstorms are analysed for the 20th century. Long term series of strong winds from the 16th century are produced using information from documentary evidence (narrative sources, visual daily weather observations, newspapers etc.). Trends in strong winds are analysed with respect to circulation characteristics (NAOI, CEZI) and winter temperatures in Central Europe. Climatology of tornadoes is presented with respect to their seasonality, spatial distribution, impacts and intensity according to Fujita scale. Higher frequency of strong winds appears in the late 16th and in the early 17th centuries. It corresponds with the common deterioration of the Central European climate. On the other hand, the lower number of recorded events during the 1940s and 1950s is connected with the quality of data excerpted mostly from newspapers for this period. Documentary evidence allows identify the most disastrous historical windstorms and provides valuable information on impacts to nature and society. In such a way information of historical climatology complement data from the instrumental period and help to define the role of anthropogenic factor in present global climate change.
Links
GA205/01/1067, research and development projectName: Meteorologické extrémy a jejich dopady v Českých zemích od 16. století
Investor: Czech Science Foundation, Meteorological extremes and their impacts in the Czech Lands since the 16th century
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