Tree-rings and people - different views on the 1540 Megadrought. Reply to Buntgen et al. 2015
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216224%3A14310%2F15%3A00081169" target="_blank" >RIV/00216224:14310/15:00081169 - isvavai.cz</a>
Výsledek na webu
<a href="http://dx.doi.org/10.1007/s10584-015-1429-8" target="_blank" >http://dx.doi.org/10.1007/s10584-015-1429-8</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1007/s10584-015-1429-8" target="_blank" >10.1007/s10584-015-1429-8</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Tree-rings and people - different views on the 1540 Megadrought. Reply to Buntgen et al. 2015
Popis výsledku v původním jazyce
Büntgen et al. (2015; hereinafter B15) present the result of new research which question the results of Wetter et al. 2014, (hereinafter W14) and Wetter et al. (2013, hereinafter W13)regarding European climate in 1540. B15 conclude from tree-ring evidence that the results based on documentary data of W14 probably overstated the intensity and duration of the 1540 drought event. W14 termed it Megadrought because of its extreme duration and spatial extent compared to other drought events in central Europe,although they note that the term is generally used for decadal rather than for single-year droughts (Seneviratne et al. 2012). We take the opportunity to recall the following issues. Firstly, when dealing with drought the complexity of this phenomenon should be kept in mind. Meteorological drought defined as a large negative precipitation anomaly during a certain period can trigger agricultural, hydrological, groundwater and socioeconomic droughts.
Název v anglickém jazyce
Tree-rings and people - different views on the 1540 Megadrought. Reply to Buntgen et al. 2015
Popis výsledku anglicky
Büntgen et al. (2015; hereinafter B15) present the result of new research which question the results of Wetter et al. 2014, (hereinafter W14) and Wetter et al. (2013, hereinafter W13)regarding European climate in 1540. B15 conclude from tree-ring evidence that the results based on documentary data of W14 probably overstated the intensity and duration of the 1540 drought event. W14 termed it Megadrought because of its extreme duration and spatial extent compared to other drought events in central Europe,although they note that the term is generally used for decadal rather than for single-year droughts (Seneviratne et al. 2012). We take the opportunity to recall the following issues. Firstly, when dealing with drought the complexity of this phenomenon should be kept in mind. Meteorological drought defined as a large negative precipitation anomaly during a certain period can trigger agricultural, hydrological, groundwater and socioeconomic droughts.
Klasifikace
Druh
O - Ostatní výsledky
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
2015
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů