Exploring Combined Influences of Seasonal East Atlantic (EA) and North Atlantic Oscillation (NAO) on the Temperature-Precipitation Relationship in the Iberian Peninsula

The combined influence of the North Atlantic Oscillation (NAO) and the East Atlantic (EA) patterns on the covariability of temperatures and precipitation in 35 stations of the Iberian Peninsula during the period 1950–2019 is analysed in this work. Four EA-NAO composites were defined from teleconnect...

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Published in:Geosciences
Main Author: Fernando S. Rodrigo
Format: Article in Journal/Newspaper
Language:English
Published: MDPI AG 2021
Subjects:
NAO
EA
Online Access:https://doi.org/10.3390/geosciences11050211
https://doaj.org/article/72771b2dade149dc86c8a889ebb2e6fd
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spelling ftdoajarticles:oai:doaj.org/article:72771b2dade149dc86c8a889ebb2e6fd 2023-05-15T17:29:57+02:00 Exploring Combined Influences of Seasonal East Atlantic (EA) and North Atlantic Oscillation (NAO) on the Temperature-Precipitation Relationship in the Iberian Peninsula Fernando S. Rodrigo 2021-05-01T00:00:00Z https://doi.org/10.3390/geosciences11050211 https://doaj.org/article/72771b2dade149dc86c8a889ebb2e6fd EN eng MDPI AG https://www.mdpi.com/2076-3263/11/5/211 https://doaj.org/toc/2076-3263 doi:10.3390/geosciences11050211 2076-3263 https://doaj.org/article/72771b2dade149dc86c8a889ebb2e6fd Geosciences, Vol 11, Iss 211, p 211 (2021) NAO EA temperature-precipitation covariability Iberian Peninsula Geology QE1-996.5 article 2021 ftdoajarticles https://doi.org/10.3390/geosciences11050211 2022-12-31T13:45:45Z The combined influence of the North Atlantic Oscillation (NAO) and the East Atlantic (EA) patterns on the covariability of temperatures and precipitation in 35 stations of the Iberian Peninsula during the period 1950–2019 is analysed in this work. Four EA-NAO composites were defined from teleconnection patterns’ positive and negative phases: EA+NAO+, EA+NAO-, EA-NAO+ and EA-NAO-. Daily data of maximum and minimum temperature were used to obtain seasonal means (TX and TN, respectively), and the covariability of these variables with accumulated seasonal rainfall (R) was studied comparing results obtained for different NAO and EA composites. Main results indicate slight differences in the spatial coverage of correlation coefficients between R and temperature variables, except in spring when the generalised negative relationship between R and TX under EA+NAO+ and EA-NAO- disappears under EA-NAO+ and EA+NAO- composites. This result may be useful to interpret and discuss historical reconstructions of the Iberian climate. Article in Journal/Newspaper North Atlantic North Atlantic oscillation Directory of Open Access Journals: DOAJ Articles Geosciences 11 5 211
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic NAO
EA
temperature-precipitation covariability
Iberian Peninsula
Geology
QE1-996.5
spellingShingle NAO
EA
temperature-precipitation covariability
Iberian Peninsula
Geology
QE1-996.5
Fernando S. Rodrigo
Exploring Combined Influences of Seasonal East Atlantic (EA) and North Atlantic Oscillation (NAO) on the Temperature-Precipitation Relationship in the Iberian Peninsula
topic_facet NAO
EA
temperature-precipitation covariability
Iberian Peninsula
Geology
QE1-996.5
description The combined influence of the North Atlantic Oscillation (NAO) and the East Atlantic (EA) patterns on the covariability of temperatures and precipitation in 35 stations of the Iberian Peninsula during the period 1950–2019 is analysed in this work. Four EA-NAO composites were defined from teleconnection patterns’ positive and negative phases: EA+NAO+, EA+NAO-, EA-NAO+ and EA-NAO-. Daily data of maximum and minimum temperature were used to obtain seasonal means (TX and TN, respectively), and the covariability of these variables with accumulated seasonal rainfall (R) was studied comparing results obtained for different NAO and EA composites. Main results indicate slight differences in the spatial coverage of correlation coefficients between R and temperature variables, except in spring when the generalised negative relationship between R and TX under EA+NAO+ and EA-NAO- disappears under EA-NAO+ and EA+NAO- composites. This result may be useful to interpret and discuss historical reconstructions of the Iberian climate.
format Article in Journal/Newspaper
author Fernando S. Rodrigo
author_facet Fernando S. Rodrigo
author_sort Fernando S. Rodrigo
title Exploring Combined Influences of Seasonal East Atlantic (EA) and North Atlantic Oscillation (NAO) on the Temperature-Precipitation Relationship in the Iberian Peninsula
title_short Exploring Combined Influences of Seasonal East Atlantic (EA) and North Atlantic Oscillation (NAO) on the Temperature-Precipitation Relationship in the Iberian Peninsula
title_full Exploring Combined Influences of Seasonal East Atlantic (EA) and North Atlantic Oscillation (NAO) on the Temperature-Precipitation Relationship in the Iberian Peninsula
title_fullStr Exploring Combined Influences of Seasonal East Atlantic (EA) and North Atlantic Oscillation (NAO) on the Temperature-Precipitation Relationship in the Iberian Peninsula
title_full_unstemmed Exploring Combined Influences of Seasonal East Atlantic (EA) and North Atlantic Oscillation (NAO) on the Temperature-Precipitation Relationship in the Iberian Peninsula
title_sort exploring combined influences of seasonal east atlantic (ea) and north atlantic oscillation (nao) on the temperature-precipitation relationship in the iberian peninsula
publisher MDPI AG
publishDate 2021
url https://doi.org/10.3390/geosciences11050211
https://doaj.org/article/72771b2dade149dc86c8a889ebb2e6fd
genre North Atlantic
North Atlantic oscillation
genre_facet North Atlantic
North Atlantic oscillation
op_source Geosciences, Vol 11, Iss 211, p 211 (2021)
op_relation https://www.mdpi.com/2076-3263/11/5/211
https://doaj.org/toc/2076-3263
doi:10.3390/geosciences11050211
2076-3263
https://doaj.org/article/72771b2dade149dc86c8a889ebb2e6fd
op_doi https://doi.org/10.3390/geosciences11050211
container_title Geosciences
container_volume 11
container_issue 5
container_start_page 211
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