Long-term trends in strong winds in the Czech Republic

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216224%3A14310%2F06%3A00029016" target="_blank" >RIV/00216224:14310/06:00029016 - isvavai.cz</a>

Výsledek na webu

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DOI - Digital Object Identifier

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Jazyk výsledku

angličtina

Název v původním jazyce

Long-term trends in strong winds in the Czech Republic

Popis výsledku v původním jazyce

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 windstormsrelated 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.

Název v anglickém jazyce

Long-term trends in strong winds in the Czech Republic

Popis výsledku anglicky

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 windstormsrelated 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.

Druh

D - Stať ve sborníku

CEP obor

DG - Vědy o atmosféře, meteorologie

OECD FORD obor

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Projekt

<a href="/cs/project/GA205%2F01%2F1067" target="_blank" >GA205/01/1067: Meteorologické extrémy a jejich dopady v Českých zemích od 16. století</a><br>

Návaznosti

P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Rok uplatnění

2006

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název statě ve sborníku

Geophysical Research Abstracts, EGU General Assembly, Vol. 8

ISBN

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ISSN

1607-7962

e-ISSN

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Počet stran výsledku

1

Strana od-do

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Název nakladatele

European Geophysical Union

Místo vydání

Vienna

Místo konání akce

Vienna

Datum konání akce

2. 4. 2006

Typ akce podle státní příslušnosti

EUR - Evropská akce

Kód UT WoS článku

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