The year-long unprecedented European heat and drought of 1540 ? a worst case
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216224%3A14310%2F14%3A00073833" target="_blank" >RIV/00216224:14310/14:00073833 - isvavai.cz</a>
Nalezeny alternativní kódy
RIV/86652079:_____/14:00496503
Výsledek na webu
<a href="http://dx.doi.org/10.1007/s10584-014-1184-2" target="_blank" >http://dx.doi.org/10.1007/s10584-014-1184-2</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1007/s10584-014-1184-2" target="_blank" >10.1007/s10584-014-1184-2</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
The year-long unprecedented European heat and drought of 1540 ? a worst case
Popis výsledku v původním jazyce
The heat waves of 2003 in Western Europe and 2010 in Russia, commonly labelled as rare climatic anomalies outside of previous experience, are often taken as harbingers of more frequent extremes in the global warming-influenced future. However, a recent reconstruction of spring?summer temperatures for WE resulted in the likelihood of significantly higher temperatures in 1540. In order to check the plausibility of this result we investigated the severity of the 1540 drought by putting forward the argumentof the known soil desiccation-temperature feedback. Based on more than 300 first-hand documentary weather report sources originating from an area of 2 to 3 million km2, we show that Europe was affected by an unprecedented 11-month-long Megadrought. Theestimated number of precipitation days and precipitation amount for Central and Western Europe in 1540 is significantly lower than the 100-year minima of the instrumental measurement period for spring, summer and autumn.
Název v anglickém jazyce
The year-long unprecedented European heat and drought of 1540 ? a worst case
Popis výsledku anglicky
The heat waves of 2003 in Western Europe and 2010 in Russia, commonly labelled as rare climatic anomalies outside of previous experience, are often taken as harbingers of more frequent extremes in the global warming-influenced future. However, a recent reconstruction of spring?summer temperatures for WE resulted in the likelihood of significantly higher temperatures in 1540. In order to check the plausibility of this result we investigated the severity of the 1540 drought by putting forward the argumentof the known soil desiccation-temperature feedback. Based on more than 300 first-hand documentary weather report sources originating from an area of 2 to 3 million km2, we show that Europe was affected by an unprecedented 11-month-long Megadrought. Theestimated number of precipitation days and precipitation amount for Central and Western Europe in 1540 is significantly lower than the 100-year minima of the instrumental measurement period for spring, summer and autumn.
Klasifikace
Druh
J<sub>x</sub> - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)
CEP obor
DG - Vědy o atmosféře, meteorologie
OECD FORD obor
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Návaznosti výsledku
Projekt
Výsledek vznikl pri realizaci vícero projektů. Více informací v záložce Projekty.
Návaznosti
P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)
Ostatní
Rok uplatnění
2014
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
Climatic Change
ISSN
0165-0009
e-ISSN
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Svazek periodika
125
Číslo periodika v rámci svazku
3-4
Stát vydavatele periodika
NL - Nizozemsko
Počet stran výsledku
15
Strana od-do
349-363
Kód UT WoS článku
000339970700005
EID výsledku v databázi Scopus
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