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
- Institución
- Consejo Nacional de Investigaciones Científicas y Técnicas
- OAI Identificador
- oai:ri.conicet.gov.ar:11336/92548
Ver los metadatos del registro completo
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 |