Increasing compound warm spells and droughts in the Mediterranean Basin
The co-occurrence of warm spells and droughts can lead to detrimental socio-economic and ecological impacts, largely surpassing the impacts of either warm spells or droughts alone. We quantify changes in the number of compound warm spells and droughts from 1979 to 2018 in the Mediterranean Basin usi...
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doaj-7a6cdb47162b4373b8ed376f6a02f8d62021-05-22T04:36:51ZengElsevierWeather and Climate Extremes2212-09472021-06-0132100312Increasing compound warm spells and droughts in the Mediterranean BasinJohannes Vogel0Eva Paton1Valentin Aich2Axel Bronstert3Institute of Environmental Science and Geography, University of Potsdam, Potsdam, Germany; Institute of Ecology, Technical University of Berlin, Berlin, Germany; Corresponding author. Institute of Environmental Science and Geography, University of Potsdam, Potsdam, Germany.Institute of Ecology, Technical University of Berlin, Berlin, GermanyPotsdam Institute for Climate Impact Research, Potsdam, GermanyInstitute of Environmental Science and Geography, University of Potsdam, Potsdam, GermanyThe co-occurrence of warm spells and droughts can lead to detrimental socio-economic and ecological impacts, largely surpassing the impacts of either warm spells or droughts alone. We quantify changes in the number of compound warm spells and droughts from 1979 to 2018 in the Mediterranean Basin using the ERA5 data set. We analyse two types of compound events: 1) warm season compound events, which are extreme in absolute terms in the warm season from May to October and 2) year-round deseasonalised compound events, which are extreme in relative terms respective to the time of the year. The number of compound events increases significantly and especially warm spells are increasing strongly – with an annual growth rates of 3.9 (3.5) % for warm season (deseasonalised) compound events and 4.6 (4.4) % for warm spells –, whereas for droughts the change is more ambiguous depending on the applied definition. Therefore, the rise in the number of compound events is primarily driven by temperature changes and not the lack of precipitation. The months July and August show the highest increases in warm season compound events, whereas the highest increases of deseasonalised compound events occur in spring and early summer. This increase in deseasonalised compound events can potentially have a significant impact on the functioning of Mediterranean ecosystems as this is the peak phase of ecosystem productivity and a vital phenophase.http://www.sciencedirect.com/science/article/pii/S2212094721000104Compound eventsWarm spellsDroughtsMediterranean basinExtreme eventsClimate change |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Johannes Vogel Eva Paton Valentin Aich Axel Bronstert |
spellingShingle |
Johannes Vogel Eva Paton Valentin Aich Axel Bronstert Increasing compound warm spells and droughts in the Mediterranean Basin Weather and Climate Extremes Compound events Warm spells Droughts Mediterranean basin Extreme events Climate change |
author_facet |
Johannes Vogel Eva Paton Valentin Aich Axel Bronstert |
author_sort |
Johannes Vogel |
title |
Increasing compound warm spells and droughts in the Mediterranean Basin |
title_short |
Increasing compound warm spells and droughts in the Mediterranean Basin |
title_full |
Increasing compound warm spells and droughts in the Mediterranean Basin |
title_fullStr |
Increasing compound warm spells and droughts in the Mediterranean Basin |
title_full_unstemmed |
Increasing compound warm spells and droughts in the Mediterranean Basin |
title_sort |
increasing compound warm spells and droughts in the mediterranean basin |
publisher |
Elsevier |
series |
Weather and Climate Extremes |
issn |
2212-0947 |
publishDate |
2021-06-01 |
description |
The co-occurrence of warm spells and droughts can lead to detrimental socio-economic and ecological impacts, largely surpassing the impacts of either warm spells or droughts alone. We quantify changes in the number of compound warm spells and droughts from 1979 to 2018 in the Mediterranean Basin using the ERA5 data set. We analyse two types of compound events: 1) warm season compound events, which are extreme in absolute terms in the warm season from May to October and 2) year-round deseasonalised compound events, which are extreme in relative terms respective to the time of the year. The number of compound events increases significantly and especially warm spells are increasing strongly – with an annual growth rates of 3.9 (3.5) % for warm season (deseasonalised) compound events and 4.6 (4.4) % for warm spells –, whereas for droughts the change is more ambiguous depending on the applied definition. Therefore, the rise in the number of compound events is primarily driven by temperature changes and not the lack of precipitation. The months July and August show the highest increases in warm season compound events, whereas the highest increases of deseasonalised compound events occur in spring and early summer. This increase in deseasonalised compound events can potentially have a significant impact on the functioning of Mediterranean ecosystems as this is the peak phase of ecosystem productivity and a vital phenophase. |
topic |
Compound events Warm spells Droughts Mediterranean basin Extreme events Climate change |
url |
http://www.sciencedirect.com/science/article/pii/S2212094721000104 |
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