Will drought events become more frequent and severe in Europe?

Autores
Spinoni, Jonathan; Vogt, Jürgen V.; Naumann, Gustavo; Barbosa, Paulo; Dosio, Alessandro
Año de publicación
2018
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
As a result of climate change in recent past and unsustainable land management, drought became one of the most impacting disasters and, with the projected global warming, it is expected to progressively cause more damages by the end of the 21st century. This study investigates changes in drought occurrence, frequency, and severity in Europe in the next decades. A combined indicator based on the predominance of the drought signal over normal/wet conditions has been used. The indicator, which combines the standardized precipitation index (SPI, which accounts for anomalous low rainfall), the standardized precipitation evapotranspiration index (SPEI, which accounts for high temperatures and scarce precipitations), and the reconnaissance drought indicator (RDI, similar to SPEI but more affected by extreme events), has been computed at 3- and 12-month accumulation scales to characterize trends in seasonal and annual events from 1981 to 2100. Climate data from 11 bias-adjusted high-resolution (0.11°) simulations from the EURO-CORDEX (coordinated regional climate downscaling experiment) have been used in the analyses. For each simulation, the frequency and severity of drought and extreme drought events for 1981–2010, 2041–2070, and 2071–2100 have been analysed. Under the moderate emission scenario (RCP4.5), droughts are projected to become increasingly more frequent and severe in the Mediterranean area, western Europe, and Northern Scandinavia, whereas the whole European continent, with the exception of Iceland, will be affected by more frequent and severe extreme droughts under the most severe emission scenario (RCP8.5), especially after 2070. Seasonally, drought frequency is projected to increase everywhere in Europe for both scenarios in spring and summer, especially over southern Europe, and less intensely in autumn; on the contrary, winter shows a decrease in drought frequency over northern Europe.
Fil: Spinoni, Jonathan. European Commission Joint Research Centre; Italia
Fil: Vogt, Jürgen V.. European Commission Joint Research Centre; Italia
Fil: Naumann, Gustavo. European Commission Joint Research Centre; Italia. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
Fil: Barbosa, Paulo. European Commission Joint Research Centre; Italia
Fil: Dosio, Alessandro. European Commission Joint Research Centre; Italia
Materia
CLIMATE PROJECTIONS
CLIMATE SCENARIOS
DROUGHT
EURO-CORDEX
EUROPE
Nivel de accesibilidad
acceso abierto
Condiciones de uso
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
Repositorio
CONICET Digital (CONICET)
Institución
Consejo Nacional de Investigaciones Científicas y Técnicas
OAI Identificador
oai:ri.conicet.gov.ar:11336/92548

id CONICETDig_be220c3dde3377f9b5b6e0ef77108727
oai_identifier_str oai:ri.conicet.gov.ar:11336/92548
network_acronym_str CONICETDig
repository_id_str 3498
network_name_str CONICET Digital (CONICET)
spelling Will drought events become more frequent and severe in Europe?Spinoni, JonathanVogt, Jürgen V.Naumann, GustavoBarbosa, PauloDosio, AlessandroCLIMATE PROJECTIONSCLIMATE SCENARIOSDROUGHTEURO-CORDEXEUROPEhttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1As a result of climate change in recent past and unsustainable land management, drought became one of the most impacting disasters and, with the projected global warming, it is expected to progressively cause more damages by the end of the 21st century. This study investigates changes in drought occurrence, frequency, and severity in Europe in the next decades. A combined indicator based on the predominance of the drought signal over normal/wet conditions has been used. The indicator, which combines the standardized precipitation index (SPI, which accounts for anomalous low rainfall), the standardized precipitation evapotranspiration index (SPEI, which accounts for high temperatures and scarce precipitations), and the reconnaissance drought indicator (RDI, similar to SPEI but more affected by extreme events), has been computed at 3- and 12-month accumulation scales to characterize trends in seasonal and annual events from 1981 to 2100. Climate data from 11 bias-adjusted high-resolution (0.11°) simulations from the EURO-CORDEX (coordinated regional climate downscaling experiment) have been used in the analyses. For each simulation, the frequency and severity of drought and extreme drought events for 1981–2010, 2041–2070, and 2071–2100 have been analysed. Under the moderate emission scenario (RCP4.5), droughts are projected to become increasingly more frequent and severe in the Mediterranean area, western Europe, and Northern Scandinavia, whereas the whole European continent, with the exception of Iceland, will be affected by more frequent and severe extreme droughts under the most severe emission scenario (RCP8.5), especially after 2070. Seasonally, drought frequency is projected to increase everywhere in Europe for both scenarios in spring and summer, especially over southern Europe, and less intensely in autumn; on the contrary, winter shows a decrease in drought frequency over northern Europe.Fil: Spinoni, Jonathan. European Commission Joint Research Centre; ItaliaFil: Vogt, Jürgen V.. European Commission Joint Research Centre; ItaliaFil: Naumann, Gustavo. European Commission Joint Research Centre; Italia. Consejo Nacional de Investigaciones Científicas y Técnicas; ArgentinaFil: Barbosa, Paulo. European Commission Joint Research Centre; ItaliaFil: Dosio, Alessandro. European Commission Joint Research Centre; ItaliaJohn Wiley & Sons Ltd2018-03info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/92548Spinoni, Jonathan; Vogt, Jürgen V.; Naumann, Gustavo; Barbosa, Paulo; Dosio, Alessandro; Will drought events become more frequent and severe in Europe?; John Wiley & Sons Ltd; International Journal of Climatology; 38; 4; 3-2018; 1718-17360899-8418CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/https://rmets.onlinelibrary.wiley.com/doi/full/10.1002/joc.5291info:eu-repo/semantics/altIdentifier/doi/10.1002/joc.5291info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-10-15T15:43:33Zoai:ri.conicet.gov.ar:11336/92548instacron:CONICETInstitucionalhttp://ri.conicet.gov.ar/Organismo científico-tecnológicoNo correspondehttp://ri.conicet.gov.ar/oai/requestdasensio@conicet.gov.ar; lcarlino@conicet.gov.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:34982025-10-15 15:43:34.018CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv Will drought events become more frequent and severe in Europe?
title Will drought events become more frequent and severe in Europe?
spellingShingle Will drought events become more frequent and severe in Europe?
Spinoni, Jonathan
CLIMATE PROJECTIONS
CLIMATE SCENARIOS
DROUGHT
EURO-CORDEX
EUROPE
title_short Will drought events become more frequent and severe in Europe?
title_full Will drought events become more frequent and severe in Europe?
title_fullStr Will drought events become more frequent and severe in Europe?
title_full_unstemmed Will drought events become more frequent and severe in Europe?
title_sort Will drought events become more frequent and severe in Europe?
dc.creator.none.fl_str_mv Spinoni, Jonathan
Vogt, Jürgen V.
Naumann, Gustavo
Barbosa, Paulo
Dosio, Alessandro
author Spinoni, Jonathan
author_facet Spinoni, Jonathan
Vogt, Jürgen V.
Naumann, Gustavo
Barbosa, Paulo
Dosio, Alessandro
author_role author
author2 Vogt, Jürgen V.
Naumann, Gustavo
Barbosa, Paulo
Dosio, Alessandro
author2_role author
author
author
author
dc.subject.none.fl_str_mv CLIMATE PROJECTIONS
CLIMATE SCENARIOS
DROUGHT
EURO-CORDEX
EUROPE
topic CLIMATE PROJECTIONS
CLIMATE SCENARIOS
DROUGHT
EURO-CORDEX
EUROPE
purl_subject.fl_str_mv https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
dc.description.none.fl_txt_mv As a result of climate change in recent past and unsustainable land management, drought became one of the most impacting disasters and, with the projected global warming, it is expected to progressively cause more damages by the end of the 21st century. This study investigates changes in drought occurrence, frequency, and severity in Europe in the next decades. A combined indicator based on the predominance of the drought signal over normal/wet conditions has been used. The indicator, which combines the standardized precipitation index (SPI, which accounts for anomalous low rainfall), the standardized precipitation evapotranspiration index (SPEI, which accounts for high temperatures and scarce precipitations), and the reconnaissance drought indicator (RDI, similar to SPEI but more affected by extreme events), has been computed at 3- and 12-month accumulation scales to characterize trends in seasonal and annual events from 1981 to 2100. Climate data from 11 bias-adjusted high-resolution (0.11°) simulations from the EURO-CORDEX (coordinated regional climate downscaling experiment) have been used in the analyses. For each simulation, the frequency and severity of drought and extreme drought events for 1981–2010, 2041–2070, and 2071–2100 have been analysed. Under the moderate emission scenario (RCP4.5), droughts are projected to become increasingly more frequent and severe in the Mediterranean area, western Europe, and Northern Scandinavia, whereas the whole European continent, with the exception of Iceland, will be affected by more frequent and severe extreme droughts under the most severe emission scenario (RCP8.5), especially after 2070. Seasonally, drought frequency is projected to increase everywhere in Europe for both scenarios in spring and summer, especially over southern Europe, and less intensely in autumn; on the contrary, winter shows a decrease in drought frequency over northern Europe.
Fil: Spinoni, Jonathan. European Commission Joint Research Centre; Italia
Fil: Vogt, Jürgen V.. European Commission Joint Research Centre; Italia
Fil: Naumann, Gustavo. European Commission Joint Research Centre; Italia. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
Fil: Barbosa, Paulo. European Commission Joint Research Centre; Italia
Fil: Dosio, Alessandro. European Commission Joint Research Centre; Italia
description As a result of climate change in recent past and unsustainable land management, drought became one of the most impacting disasters and, with the projected global warming, it is expected to progressively cause more damages by the end of the 21st century. This study investigates changes in drought occurrence, frequency, and severity in Europe in the next decades. A combined indicator based on the predominance of the drought signal over normal/wet conditions has been used. The indicator, which combines the standardized precipitation index (SPI, which accounts for anomalous low rainfall), the standardized precipitation evapotranspiration index (SPEI, which accounts for high temperatures and scarce precipitations), and the reconnaissance drought indicator (RDI, similar to SPEI but more affected by extreme events), has been computed at 3- and 12-month accumulation scales to characterize trends in seasonal and annual events from 1981 to 2100. Climate data from 11 bias-adjusted high-resolution (0.11°) simulations from the EURO-CORDEX (coordinated regional climate downscaling experiment) have been used in the analyses. For each simulation, the frequency and severity of drought and extreme drought events for 1981–2010, 2041–2070, and 2071–2100 have been analysed. Under the moderate emission scenario (RCP4.5), droughts are projected to become increasingly more frequent and severe in the Mediterranean area, western Europe, and Northern Scandinavia, whereas the whole European continent, with the exception of Iceland, will be affected by more frequent and severe extreme droughts under the most severe emission scenario (RCP8.5), especially after 2070. Seasonally, drought frequency is projected to increase everywhere in Europe for both scenarios in spring and summer, especially over southern Europe, and less intensely in autumn; on the contrary, winter shows a decrease in drought frequency over northern Europe.
publishDate 2018
dc.date.none.fl_str_mv 2018-03
dc.type.none.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
http://purl.org/coar/resource_type/c_6501
info:ar-repo/semantics/articulo
format article
status_str publishedVersion
dc.identifier.none.fl_str_mv http://hdl.handle.net/11336/92548
Spinoni, Jonathan; Vogt, Jürgen V.; Naumann, Gustavo; Barbosa, Paulo; Dosio, Alessandro; Will drought events become more frequent and severe in Europe?; John Wiley & Sons Ltd; International Journal of Climatology; 38; 4; 3-2018; 1718-1736
0899-8418
CONICET Digital
CONICET
url http://hdl.handle.net/11336/92548
identifier_str_mv Spinoni, Jonathan; Vogt, Jürgen V.; Naumann, Gustavo; Barbosa, Paulo; Dosio, Alessandro; Will drought events become more frequent and severe in Europe?; John Wiley & Sons Ltd; International Journal of Climatology; 38; 4; 3-2018; 1718-1736
0899-8418
CONICET Digital
CONICET
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/url/https://rmets.onlinelibrary.wiley.com/doi/full/10.1002/joc.5291
info:eu-repo/semantics/altIdentifier/doi/10.1002/joc.5291
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
eu_rights_str_mv openAccess
rights_invalid_str_mv https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
dc.format.none.fl_str_mv application/pdf
application/pdf
dc.publisher.none.fl_str_mv John Wiley & Sons Ltd
publisher.none.fl_str_mv John Wiley & Sons Ltd
dc.source.none.fl_str_mv reponame:CONICET Digital (CONICET)
instname:Consejo Nacional de Investigaciones Científicas y Técnicas
reponame_str CONICET Digital (CONICET)
collection CONICET Digital (CONICET)
instname_str Consejo Nacional de Investigaciones Científicas y Técnicas
repository.name.fl_str_mv CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicas
repository.mail.fl_str_mv dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar
_version_ 1846083540468367360
score 13.216834