Flow dependence of wintertime subseasonal prediction skill over Europe

Issuing skillful forecasts beyond the typical horizon of weather predictability remains a challenge actively addressed by the scientific community. This study evaluates winter subseasonal reforecasts delivered by the CNRM and ECMWF dynamical systems and identifies that the level of skill for predict...

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Published in:Weather and Climate Dynamics
Main Authors: Ardilouze, Constantin, Specq, Damien, Batté, Lauriane, Cassou, Christophe
Format: Text
Language:English
Published: 2021
Subjects:
Online Access:https://doi.org/10.5194/wcd-2-1033-2021
https://wcd.copernicus.org/articles/2/1033/2021/
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spelling ftcopernicus:oai:publications.copernicus.org:wcd95008 2023-05-15T17:33:32+02:00 Flow dependence of wintertime subseasonal prediction skill over Europe Ardilouze, Constantin Specq, Damien Batté, Lauriane Cassou, Christophe 2021-11-04 application/pdf https://doi.org/10.5194/wcd-2-1033-2021 https://wcd.copernicus.org/articles/2/1033/2021/ eng eng doi:10.5194/wcd-2-1033-2021 https://wcd.copernicus.org/articles/2/1033/2021/ eISSN: 2698-4016 Text 2021 ftcopernicus https://doi.org/10.5194/wcd-2-1033-2021 2021-11-08T17:22:29Z Issuing skillful forecasts beyond the typical horizon of weather predictability remains a challenge actively addressed by the scientific community. This study evaluates winter subseasonal reforecasts delivered by the CNRM and ECMWF dynamical systems and identifies that the level of skill for predicting temperature in Europe varies fairly consistently in both systems. In particular, forecasts initialized during positive North Atlantic Oscillation (NAO) phases tend to be more skillful over Europe at week 3 in both systems. Composite analyses performed in an atmospheric reanalysis, a long-term climate simulation and both forecast systems unveil very similar temperature and sea-level pressure patterns 3 weeks after NAO conditions. Furthermore, regressing these fields onto the 3-weeks-prior NAO index in a reanalysis shows consistent patterns over Europe but also other regions of the Northern Hemisphere extratropics, thereby suggesting a lagged teleconnection, related to either the persistence or recurrence of the positive and negative phases of the NAO. This teleconnection, conditioned to the intensity of the initial NAO phase, is well captured by forecast systems. As a result, it is a key mechanism for determining a priori confidence in the skill of wintertime subseasonal forecasts over Europe as well as other parts of the Northern Hemisphere. Text North Atlantic North Atlantic oscillation Copernicus Publications: E-Journals Weather and Climate Dynamics 2 4 1033 1049
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description Issuing skillful forecasts beyond the typical horizon of weather predictability remains a challenge actively addressed by the scientific community. This study evaluates winter subseasonal reforecasts delivered by the CNRM and ECMWF dynamical systems and identifies that the level of skill for predicting temperature in Europe varies fairly consistently in both systems. In particular, forecasts initialized during positive North Atlantic Oscillation (NAO) phases tend to be more skillful over Europe at week 3 in both systems. Composite analyses performed in an atmospheric reanalysis, a long-term climate simulation and both forecast systems unveil very similar temperature and sea-level pressure patterns 3 weeks after NAO conditions. Furthermore, regressing these fields onto the 3-weeks-prior NAO index in a reanalysis shows consistent patterns over Europe but also other regions of the Northern Hemisphere extratropics, thereby suggesting a lagged teleconnection, related to either the persistence or recurrence of the positive and negative phases of the NAO. This teleconnection, conditioned to the intensity of the initial NAO phase, is well captured by forecast systems. As a result, it is a key mechanism for determining a priori confidence in the skill of wintertime subseasonal forecasts over Europe as well as other parts of the Northern Hemisphere.
format Text
author Ardilouze, Constantin
Specq, Damien
Batté, Lauriane
Cassou, Christophe
spellingShingle Ardilouze, Constantin
Specq, Damien
Batté, Lauriane
Cassou, Christophe
Flow dependence of wintertime subseasonal prediction skill over Europe
author_facet Ardilouze, Constantin
Specq, Damien
Batté, Lauriane
Cassou, Christophe
author_sort Ardilouze, Constantin
title Flow dependence of wintertime subseasonal prediction skill over Europe
title_short Flow dependence of wintertime subseasonal prediction skill over Europe
title_full Flow dependence of wintertime subseasonal prediction skill over Europe
title_fullStr Flow dependence of wintertime subseasonal prediction skill over Europe
title_full_unstemmed Flow dependence of wintertime subseasonal prediction skill over Europe
title_sort flow dependence of wintertime subseasonal prediction skill over europe
publishDate 2021
url https://doi.org/10.5194/wcd-2-1033-2021
https://wcd.copernicus.org/articles/2/1033/2021/
genre North Atlantic
North Atlantic oscillation
genre_facet North Atlantic
North Atlantic oscillation
op_source eISSN: 2698-4016
op_relation doi:10.5194/wcd-2-1033-2021
https://wcd.copernicus.org/articles/2/1033/2021/
op_doi https://doi.org/10.5194/wcd-2-1033-2021
container_title Weather and Climate Dynamics
container_volume 2
container_issue 4
container_start_page 1033
op_container_end_page 1049
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