Subseasonal temperature trends in Europe (1961-2000) and their links to atmospheric circulation

Kód výsledku v IS VaVaI

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Nalezeny alternativní kódy

RIV/68378289:_____/13:00422715

Výsledek na webu

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DOI - Digital Object Identifier

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Jazyk výsledku

angličtina

Název v původním jazyce

Subseasonal temperature trends in Europe (1961-2000) and their links to atmospheric circulation

Popis výsledku v původním jazyce

We use daily maximum and minimum temperatures and the daily temperature range from 136 stations in Europe in the period 1961?2000 to precisely locate their seasonal and subseasonal trends within the year. Linear trends are calculated for moving ?subseasons of 10, 20, 30, 60, and 90 days, each shifted by one day. Over most of Europe, the observed warming is greatest in winter. In Iceland and the Mediterranean, a pronounced warming is only present in summer. Significant autumn cooling was found in Easternand Southeastern Europe for both TX and TN. Other non-warming periods occur in Western and Central Europe in February, April, and late June. Trends of DTR are inconclusive. Changes in the frequency of atmospheric circulation types usually explain a substantial part of the observed climatic trends; however, the influence varies between regions, times of the year, subseason lengths, numbers of circulation types, and input variables for the classification of circulation types.

Název v anglickém jazyce

Subseasonal temperature trends in Europe (1961-2000) and their links to atmospheric circulation

Popis výsledku anglicky

We use daily maximum and minimum temperatures and the daily temperature range from 136 stations in Europe in the period 1961?2000 to precisely locate their seasonal and subseasonal trends within the year. Linear trends are calculated for moving ?subseasons of 10, 20, 30, 60, and 90 days, each shifted by one day. Over most of Europe, the observed warming is greatest in winter. In Iceland and the Mediterranean, a pronounced warming is only present in summer. Significant autumn cooling was found in Easternand Southeastern Europe for both TX and TN. Other non-warming periods occur in Western and Central Europe in February, April, and late June. Trends of DTR are inconclusive. Changes in the frequency of atmospheric circulation types usually explain a substantial part of the observed climatic trends; however, the influence varies between regions, times of the year, subseason lengths, numbers of circulation types, and input variables for the classification of circulation types.

Druh

D - Stať ve sborníku

CEP obor

EH - Ekologie – společenstva

OECD FORD obor

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Projekt

Výsledek vznikl pri realizaci vícero projektů. Více informací v záložce Projekty.

Návaznosti

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2013

Kód důvěrnosti údajů

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

Název statě ve sborníku

Global Change and Resilience: From Impacts to Responses : Proceedings of the 3rd annual Global Change and Resilience Conference

ISBN

978-80-904351-8-6

ISSN

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e-ISSN

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Počet stran výsledku

5

Strana od-do

90-94

Název nakladatele

Global change research centre, Academy of Sciences of the Czech Republic, v. v. i

Místo vydání

Brno

Místo konání akce

Brno

Datum konání akce

22. 5. 2013

Typ akce podle státní příslušnosti

EUR - Evropská akce

Kód UT WoS článku

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