Anthropogenic warming exacerbates European soil moisture droughts
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F60460709%3A41330%2F18%3A76465" target="_blank" >RIV/60460709:41330/18:76465 - isvavai.cz</a>
Výsledek na webu
<a href="http://dx.doi.org/10.1038/s41558-018-0138-5" target="_blank" >http://dx.doi.org/10.1038/s41558-018-0138-5</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1038/s41558-018-0138-5" target="_blank" >10.1038/s41558-018-0138-5</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Anthropogenic warming exacerbates European soil moisture droughts
Popis výsledku v původním jazyce
Anthropogenic warming is anticipated to increase soil moisture drought in the future. However, projections are accompanied by large uncertainty due to varying estimates of future warming. Here, using an ensemble of hydrological and land surface models, forced with bias corrected downscaled general circulation model output, we estimate the impacts from 1K to 3K global mean temperature increases on soil moisture droughts in Europe. Compared to the 1,5K Paris target, an increase of 3K, which represents current projected temperature change, is found to increase drought area by 40percent (plus minus 24 percent), affecting up to 42percent (plus minus 22percent) more of the population. Furthermore, an event similar to the 2003 drought is shown to become twice as frequent, thus, due to their increased occurrence, events of this magnitude will no longer be classified as extreme. In the absence of effective mitigation, Europe will therefore face unprecedented increases in soil moisture drought, presenting new
Název v anglickém jazyce
Anthropogenic warming exacerbates European soil moisture droughts
Popis výsledku anglicky
Anthropogenic warming is anticipated to increase soil moisture drought in the future. However, projections are accompanied by large uncertainty due to varying estimates of future warming. Here, using an ensemble of hydrological and land surface models, forced with bias corrected downscaled general circulation model output, we estimate the impacts from 1K to 3K global mean temperature increases on soil moisture droughts in Europe. Compared to the 1,5K Paris target, an increase of 3K, which represents current projected temperature change, is found to increase drought area by 40percent (plus minus 24 percent), affecting up to 42percent (plus minus 22percent) more of the population. Furthermore, an event similar to the 2003 drought is shown to become twice as frequent, thus, due to their increased occurrence, events of this magnitude will no longer be classified as extreme. In the absence of effective mitigation, Europe will therefore face unprecedented increases in soil moisture drought, presenting new
Klasifikace
Druh
J<sub>imp</sub> - Článek v periodiku v databázi Web of Science
CEP obor
—
OECD FORD obor
10501 - Hydrology
Návaznosti výsledku
Projekt
—
Návaznosti
S - Specificky vyzkum na vysokych skolach
Ostatní
Rok uplatnění
2018
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
Nature Climate Change
ISSN
1758-678x
e-ISSN
1758-678X
Svazek periodika
8
Číslo periodika v rámci svazku
5
Stát vydavatele periodika
GB - Spojené království Velké Británie a Severního Irska
Počet stran výsledku
6
Strana od-do
421-426
Kód UT WoS článku
000431139900026
EID výsledku v databázi Scopus
2-s2.0-85045837734