Decadal predictability of late winter precipitation in western Europe through an ocean–jet stream connection

The characteristics of the North Atlantic jet stream play a key role in the weather and climate of western Europe. Although much of the year-to-year variability in the jet stream arises from internal atmospheric processes that are inherently unpredictable on timescales beyond a few days to weeks, an...

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Published in:Nature Geoscience
Other Authors: Simpson, Isla R. (author), Yeager, Stephen G. (author), McKinnon, Karen A. (author), Deser, Clara (author)
Format: Article in Journal/Newspaper
Language:English
Published: 2019
Subjects:
Online Access:https://doi.org/10.1038/s41561-019-0391-x
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spelling ftncar:oai:drupal-site.org:articles_22708 2023-09-05T13:21:26+02:00 Decadal predictability of late winter precipitation in western Europe through an ocean–jet stream connection Simpson, Isla R. (author) Yeager, Stephen G. (author) McKinnon, Karen A. (author) Deser, Clara (author) 2019-08-08 https://doi.org/10.1038/s41561-019-0391-x en eng Nature Geoscience--Nat. Geosci.--1752-0894--1752-0908 articles:22708 ark:/85065/d75q4xvt doi:10.1038/s41561-019-0391-x Copyright 2019 Author(s), under exclusive license to Springer Nature Limited. article Text 2019 ftncar https://doi.org/10.1038/s41561-019-0391-x 2023-08-14T18:50:27Z The characteristics of the North Atlantic jet stream play a key role in the weather and climate of western Europe. Although much of the year-to-year variability in the jet stream arises from internal atmospheric processes that are inherently unpredictable on timescales beyond a few days to weeks, any low-frequency variability or long-term trends that can be considered forced by slowly varying boundary conditions offer the potential for extended range predictability of climatological conditions in western Europe. Here we demonstrate that station-based precipitation observations have displayed pronounced multidecadal variability over the past century in western Europe during the late winter. We then use these precipitation observations as an independent verification of the multidecadal Atlantic jet stream variability found in reanalysis products. Both signals are highly correlated with sea surface temperature variability in the North Atlantic that is well predicted in initialized decadal prediction experiments with a coupled general circulation model. Combining the model-based predictions of the sea surface temperature with the observed relationship between precipitation and sea surface temperature, we show that there is great potential for skilful predictions of the forthcoming decadal average of March precipitation in western Europe, with hindcasts for the UK and Portugal yielding anomaly correlation coefficients of 0.82 and 0.69, respectively. 1852977 OCE1243015 Article in Journal/Newspaper North Atlantic OpenSky (NCAR/UCAR - National Center for Atmospheric Research/University Corporation for Atmospheric Research) Nature Geoscience 12 8 613 619
institution Open Polar
collection OpenSky (NCAR/UCAR - National Center for Atmospheric Research/University Corporation for Atmospheric Research)
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language English
description The characteristics of the North Atlantic jet stream play a key role in the weather and climate of western Europe. Although much of the year-to-year variability in the jet stream arises from internal atmospheric processes that are inherently unpredictable on timescales beyond a few days to weeks, any low-frequency variability or long-term trends that can be considered forced by slowly varying boundary conditions offer the potential for extended range predictability of climatological conditions in western Europe. Here we demonstrate that station-based precipitation observations have displayed pronounced multidecadal variability over the past century in western Europe during the late winter. We then use these precipitation observations as an independent verification of the multidecadal Atlantic jet stream variability found in reanalysis products. Both signals are highly correlated with sea surface temperature variability in the North Atlantic that is well predicted in initialized decadal prediction experiments with a coupled general circulation model. Combining the model-based predictions of the sea surface temperature with the observed relationship between precipitation and sea surface temperature, we show that there is great potential for skilful predictions of the forthcoming decadal average of March precipitation in western Europe, with hindcasts for the UK and Portugal yielding anomaly correlation coefficients of 0.82 and 0.69, respectively. 1852977 OCE1243015
author2 Simpson, Isla R. (author)
Yeager, Stephen G. (author)
McKinnon, Karen A. (author)
Deser, Clara (author)
format Article in Journal/Newspaper
title Decadal predictability of late winter precipitation in western Europe through an ocean–jet stream connection
spellingShingle Decadal predictability of late winter precipitation in western Europe through an ocean–jet stream connection
title_short Decadal predictability of late winter precipitation in western Europe through an ocean–jet stream connection
title_full Decadal predictability of late winter precipitation in western Europe through an ocean–jet stream connection
title_fullStr Decadal predictability of late winter precipitation in western Europe through an ocean–jet stream connection
title_full_unstemmed Decadal predictability of late winter precipitation in western Europe through an ocean–jet stream connection
title_sort decadal predictability of late winter precipitation in western europe through an ocean–jet stream connection
publishDate 2019
url https://doi.org/10.1038/s41561-019-0391-x
genre North Atlantic
genre_facet North Atlantic
op_relation Nature Geoscience--Nat. Geosci.--1752-0894--1752-0908
articles:22708
ark:/85065/d75q4xvt
doi:10.1038/s41561-019-0391-x
op_rights Copyright 2019 Author(s), under exclusive license to Springer Nature Limited.
op_doi https://doi.org/10.1038/s41561-019-0391-x
container_title Nature Geoscience
container_volume 12
container_issue 8
container_start_page 613
op_container_end_page 619
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