Is the decadal variability in the tropical Atlantic a precursor to the NAO?

In the past two decades climate research in the tropical Atlantic with respect to the inter-hemispheric gradient of sea surface temperature (SST) emphasized the predominance of decadal-scale variability. Our results show that this mode of variability is prevalent only for part of the last 130-years...

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Published in:Annales Geophysicae
Main Authors: Wainer, I., Servain, J., Clauzet, G.
Format: Text
Language:English
Published: 2018
Subjects:
Online Access:https://doi.org/10.5194/angeo-26-4075-2008
https://angeo.copernicus.org/articles/26/4075/2008/
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spelling ftcopernicus:oai:publications.copernicus.org:angeo36632 2023-05-15T17:31:44+02:00 Is the decadal variability in the tropical Atlantic a precursor to the NAO? Wainer, I. Servain, J. Clauzet, G. 2018-09-27 application/pdf https://doi.org/10.5194/angeo-26-4075-2008 https://angeo.copernicus.org/articles/26/4075/2008/ eng eng doi:10.5194/angeo-26-4075-2008 https://angeo.copernicus.org/articles/26/4075/2008/ eISSN: 1432-0576 Text 2018 ftcopernicus https://doi.org/10.5194/angeo-26-4075-2008 2020-07-20T16:26:45Z In the past two decades climate research in the tropical Atlantic with respect to the inter-hemispheric gradient of sea surface temperature (SST) emphasized the predominance of decadal-scale variability. Our results show that this mode of variability is prevalent only for part of the last 130-years record (the 1880s, the 1920s and, especially, the 1970s). There is a lag of a few months between the decadal variations of the inter-hemispheric gradient of SST and the decadal variability of the North Atlantic Oscillation (NAO). This seems to indicate that the 10-year variability first develops in the tropics and then propagates polewards. The inter-hemispheric gradient of SST mode should be thought as episodic and not as a periodic oscillation. Text North Atlantic North Atlantic oscillation Copernicus Publications: E-Journals Annales Geophysicae 26 12 4075 4080
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description In the past two decades climate research in the tropical Atlantic with respect to the inter-hemispheric gradient of sea surface temperature (SST) emphasized the predominance of decadal-scale variability. Our results show that this mode of variability is prevalent only for part of the last 130-years record (the 1880s, the 1920s and, especially, the 1970s). There is a lag of a few months between the decadal variations of the inter-hemispheric gradient of SST and the decadal variability of the North Atlantic Oscillation (NAO). This seems to indicate that the 10-year variability first develops in the tropics and then propagates polewards. The inter-hemispheric gradient of SST mode should be thought as episodic and not as a periodic oscillation.
format Text
author Wainer, I.
Servain, J.
Clauzet, G.
spellingShingle Wainer, I.
Servain, J.
Clauzet, G.
Is the decadal variability in the tropical Atlantic a precursor to the NAO?
author_facet Wainer, I.
Servain, J.
Clauzet, G.
author_sort Wainer, I.
title Is the decadal variability in the tropical Atlantic a precursor to the NAO?
title_short Is the decadal variability in the tropical Atlantic a precursor to the NAO?
title_full Is the decadal variability in the tropical Atlantic a precursor to the NAO?
title_fullStr Is the decadal variability in the tropical Atlantic a precursor to the NAO?
title_full_unstemmed Is the decadal variability in the tropical Atlantic a precursor to the NAO?
title_sort is the decadal variability in the tropical atlantic a precursor to the nao?
publishDate 2018
url https://doi.org/10.5194/angeo-26-4075-2008
https://angeo.copernicus.org/articles/26/4075/2008/
genre North Atlantic
North Atlantic oscillation
genre_facet North Atlantic
North Atlantic oscillation
op_source eISSN: 1432-0576
op_relation doi:10.5194/angeo-26-4075-2008
https://angeo.copernicus.org/articles/26/4075/2008/
op_doi https://doi.org/10.5194/angeo-26-4075-2008
container_title Annales Geophysicae
container_volume 26
container_issue 12
container_start_page 4075
op_container_end_page 4080
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