New monthly indices for the East Atlantic and the Scandinavian patterns beyond the 20th century

Climate variability in the North Atlantic sector is commonly ascribed to the North Atlantic Oscillation. However, recent studies have shown that taking into account the second and third mode of variability (namely the East Atlantic ¿ EA ¿ and the Scandinavian ¿ SCA ¿ patterns) greatly improves our u...

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Main Authors: Comas-Bru, Laia, Hernández, Armand
Other Authors: Ministerio de Economía y Competitividad (España)
Format: Still Image
Language:unknown
Published: 2019
Subjects:
Online Access:http://hdl.handle.net/10261/203607
https://doi.org/10.13039/501100003329
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spelling ftcsic:oai:digital.csic.es:10261/203607 2024-02-11T10:06:16+01:00 New monthly indices for the East Atlantic and the Scandinavian patterns beyond the 20th century Comas-Bru, Laia Hernández, Armand Ministerio de Economía y Competitividad (España) 2019-07-25 http://hdl.handle.net/10261/203607 https://doi.org/10.13039/501100003329 unknown #PLACEHOLDER_PARENT_METADATA_VALUE# info:eu-repo/grantAgreement/MINECO/Plan Estatal de Investigación Científica y Técnica y de Innovación 2013-2016/CGL2016-75281-C2 Publisher's version https://app.oxfordabstracts.com/events/574/program-app/submission/91794 Sí http://hdl.handle.net/10261/203607 http://dx.doi.org/10.13039/501100003329 open póster de congreso http://purl.org/coar/resource_type/c_6670 2019 ftcsic https://doi.org/10.13039/501100003329 2024-01-16T10:49:55Z Climate variability in the North Atlantic sector is commonly ascribed to the North Atlantic Oscillation. However, recent studies have shown that taking into account the second and third mode of variability (namely the East Atlantic ¿ EA ¿ and the Scandinavian ¿ SCA ¿ patterns) greatly improves our understanding of their controlling mechanisms, as well as their impact on climate. The most commonly used EA and SCA indices span the period from 1950 to present, which is too short, for example, to calibrate palaeoclimate records or assess their variability over multi-decadal scales. To tackle this, here, we create new EOF-based (empirical orthogonal function) monthly EA and SCA indices covering the period from 1851 to present, and compare them with their equivalent instrumental indices. We also review and discuss the value of these new records and provide insights into the reasons why different sources of data may give slightly different time series. Furthermore, we demonstrate that using these patterns to explain climate variability beyond the winter season needs to be done carefully due to their non-stationary behaviour. The datasets are available at https://doi.org/10.1594/PANGAEA.892769. This research was partly funded through a Beatriu de Pinós-Marie Curie COFUND contract within the framework of the FLOODES2k (2016 BP 00023), PaleoModes (CGL2016-75281-C2), and HOLMODRIVE (PTDC/CTA-GEO/29029/2018) projects. Still Image North Atlantic North Atlantic oscillation Digital.CSIC (Spanish National Research Council)
institution Open Polar
collection Digital.CSIC (Spanish National Research Council)
op_collection_id ftcsic
language unknown
description Climate variability in the North Atlantic sector is commonly ascribed to the North Atlantic Oscillation. However, recent studies have shown that taking into account the second and third mode of variability (namely the East Atlantic ¿ EA ¿ and the Scandinavian ¿ SCA ¿ patterns) greatly improves our understanding of their controlling mechanisms, as well as their impact on climate. The most commonly used EA and SCA indices span the period from 1950 to present, which is too short, for example, to calibrate palaeoclimate records or assess their variability over multi-decadal scales. To tackle this, here, we create new EOF-based (empirical orthogonal function) monthly EA and SCA indices covering the period from 1851 to present, and compare them with their equivalent instrumental indices. We also review and discuss the value of these new records and provide insights into the reasons why different sources of data may give slightly different time series. Furthermore, we demonstrate that using these patterns to explain climate variability beyond the winter season needs to be done carefully due to their non-stationary behaviour. The datasets are available at https://doi.org/10.1594/PANGAEA.892769. This research was partly funded through a Beatriu de Pinós-Marie Curie COFUND contract within the framework of the FLOODES2k (2016 BP 00023), PaleoModes (CGL2016-75281-C2), and HOLMODRIVE (PTDC/CTA-GEO/29029/2018) projects.
author2 Ministerio de Economía y Competitividad (España)
format Still Image
author Comas-Bru, Laia
Hernández, Armand
spellingShingle Comas-Bru, Laia
Hernández, Armand
New monthly indices for the East Atlantic and the Scandinavian patterns beyond the 20th century
author_facet Comas-Bru, Laia
Hernández, Armand
author_sort Comas-Bru, Laia
title New monthly indices for the East Atlantic and the Scandinavian patterns beyond the 20th century
title_short New monthly indices for the East Atlantic and the Scandinavian patterns beyond the 20th century
title_full New monthly indices for the East Atlantic and the Scandinavian patterns beyond the 20th century
title_fullStr New monthly indices for the East Atlantic and the Scandinavian patterns beyond the 20th century
title_full_unstemmed New monthly indices for the East Atlantic and the Scandinavian patterns beyond the 20th century
title_sort new monthly indices for the east atlantic and the scandinavian patterns beyond the 20th century
publishDate 2019
url http://hdl.handle.net/10261/203607
https://doi.org/10.13039/501100003329
genre North Atlantic
North Atlantic oscillation
genre_facet North Atlantic
North Atlantic oscillation
op_relation #PLACEHOLDER_PARENT_METADATA_VALUE#
info:eu-repo/grantAgreement/MINECO/Plan Estatal de Investigación Científica y Técnica y de Innovación 2013-2016/CGL2016-75281-C2
Publisher's version
https://app.oxfordabstracts.com/events/574/program-app/submission/91794

http://hdl.handle.net/10261/203607
http://dx.doi.org/10.13039/501100003329
op_rights open
op_doi https://doi.org/10.13039/501100003329
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