NAO influence on extreme winter temperatures in Madrid (Spain)

Extremely cold days (ECDs), with minimum temperatures lower than -4.6°C, have been analysed for Madrid. This threshold corresponds to the 5th percentile of the period 1963-1999. Adopting a case analysis approach, five synoptic patterns have been identified that produce these extremely low temperatur...

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Detalhes bibliográficos
Autores: Prieto, L., García Herrera, Ricardo Francisco, Díaz, J., Hernández Martín, Emiliano, Teso, T. del
Formato: artículo
Fecha de publicación:2002
País:España
Recursos:Universidad Complutense de Madrid (UCM)
Repositorio:Docta Complutense
Idioma:inglés
OAI Identifier:oai:docta.ucm.es:20.500.14352/59840
Acesso em linha:https://hdl.handle.net/20.500.14352/59840
Access Level:acceso abierto
Palavra-chave:52
North-Atlantic oscillation
Minimum temperature
Trends
Mortality
Climate
Variability
Maximum
Astrofísica
Astronomía (Física)
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repository_id_str
spelling NAO influence on extreme winter temperatures in Madrid (Spain)Prieto, L.García Herrera, Ricardo FranciscoDíaz, J.Hernández Martín, EmilianoTeso, T. del52North-Atlantic oscillationMinimum temperatureTrendsMortalityClimateVariabilityMaximumAstrofísicaAstronomía (Física)Extremely cold days (ECDs), with minimum temperatures lower than -4.6°C, have been analysed for Madrid. This threshold corresponds to the 5th percentile of the period 1963-1999. Adopting a case analysis approach, five synoptic patterns have been identified that produce these extremely low temperatures. Three of them are associated with cold air flows over the Iberian Peninsula, and the other two with a lack of significant circulation over the region. A non-linear association with the North Atlantic Oscillation (NAO) has been identified using log-linear models. The NAO positive phase leads to an increase in the winter frequency of those synoptic patterns associated with stagnant air flow over Iberia, while those characterised by cold, northern flows do not appear to be similarly influenced.European Geophysical SocietyUniversidad Complutense de Madrid20022002-12-0120022002-12-01journal articlehttp://purl.org/coar/resource_type/c_6501info:eu-repo/semantics/articleapplication/pdfhttps://hdl.handle.net/20.500.14352/59840reponame:Docta Complutenseinstname:Universidad Complutense de Madrid (UCM)Inglésengopen accesshttp://purl.org/coar/access_right/c_abf2info:eu-repo/semantics/openAccessoai:docta.ucm.es:20.500.14352/598402026-06-02T12:44:21Z
dc.title.none.fl_str_mv NAO influence on extreme winter temperatures in Madrid (Spain)
title NAO influence on extreme winter temperatures in Madrid (Spain)
spellingShingle NAO influence on extreme winter temperatures in Madrid (Spain)
Prieto, L.
52
North-Atlantic oscillation
Minimum temperature
Trends
Mortality
Climate
Variability
Maximum
Astrofísica
Astronomía (Física)
title_short NAO influence on extreme winter temperatures in Madrid (Spain)
title_full NAO influence on extreme winter temperatures in Madrid (Spain)
title_fullStr NAO influence on extreme winter temperatures in Madrid (Spain)
title_full_unstemmed NAO influence on extreme winter temperatures in Madrid (Spain)
title_sort NAO influence on extreme winter temperatures in Madrid (Spain)
dc.creator.none.fl_str_mv Prieto, L.
García Herrera, Ricardo Francisco
Díaz, J.
Hernández Martín, Emiliano
Teso, T. del
author Prieto, L.
author_facet Prieto, L.
García Herrera, Ricardo Francisco
Díaz, J.
Hernández Martín, Emiliano
Teso, T. del
author_role author
author2 García Herrera, Ricardo Francisco
Díaz, J.
Hernández Martín, Emiliano
Teso, T. del
author2_role author
author
author
author
dc.contributor.none.fl_str_mv Universidad Complutense de Madrid
dc.subject.none.fl_str_mv 52
North-Atlantic oscillation
Minimum temperature
Trends
Mortality
Climate
Variability
Maximum
Astrofísica
Astronomía (Física)
topic 52
North-Atlantic oscillation
Minimum temperature
Trends
Mortality
Climate
Variability
Maximum
Astrofísica
Astronomía (Física)
description Extremely cold days (ECDs), with minimum temperatures lower than -4.6°C, have been analysed for Madrid. This threshold corresponds to the 5th percentile of the period 1963-1999. Adopting a case analysis approach, five synoptic patterns have been identified that produce these extremely low temperatures. Three of them are associated with cold air flows over the Iberian Peninsula, and the other two with a lack of significant circulation over the region. A non-linear association with the North Atlantic Oscillation (NAO) has been identified using log-linear models. The NAO positive phase leads to an increase in the winter frequency of those synoptic patterns associated with stagnant air flow over Iberia, while those characterised by cold, northern flows do not appear to be similarly influenced.
publishDate 2002
dc.date.none.fl_str_mv 2002
2002-12-01
2002
2002-12-01
dc.type.none.fl_str_mv journal article
http://purl.org/coar/resource_type/c_6501
dc.type.openaire.fl_str_mv info:eu-repo/semantics/article
format article
dc.identifier.none.fl_str_mv https://hdl.handle.net/20.500.14352/59840
url https://hdl.handle.net/20.500.14352/59840
dc.language.none.fl_str_mv Inglés
eng
language_invalid_str_mv Inglés
language eng
dc.rights.none.fl_str_mv open access
http://purl.org/coar/access_right/c_abf2
dc.rights.openaire.fl_str_mv info:eu-repo/semantics/openAccess
rights_invalid_str_mv open access
http://purl.org/coar/access_right/c_abf2
eu_rights_str_mv openAccess
dc.format.none.fl_str_mv application/pdf
dc.publisher.none.fl_str_mv European Geophysical Society
publisher.none.fl_str_mv European Geophysical Society
dc.source.none.fl_str_mv reponame:Docta Complutense
instname:Universidad Complutense de Madrid (UCM)
instname_str Universidad Complutense de Madrid (UCM)
reponame_str Docta Complutense
collection Docta Complutense
repository.name.fl_str_mv
repository.mail.fl_str_mv
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score 15,301629