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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Main Authors: Johannes Vogel, Eva Paton, Valentin Aich, Axel Bronstert
Format: Article
Language:English
Published: Elsevier 2021-06-01
Series:Weather and Climate Extremes
Subjects:
Online Access:http://www.sciencedirect.com/science/article/pii/S2212094721000104
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spelling 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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