Quantifying climate model representation of the wintertime Euro-Atlantic circulation using geopotential-jet regimes

Even the most advanced climate models struggle to reproduce the observed wintertime circulation of the atmosphere over the North Atlantic and western Europe. During winter, the large-scale motions of this particularly challenging region are dominated by eddy-driven and highly non-linear flows, whose...

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Published in:Weather and Climate Dynamics
Main Authors: Dorrington, Joshua, Strommen, Kristian, Fabiano, Federico
Format: Text
Language:English
Published: 2022
Subjects:
Online Access:https://doi.org/10.5194/wcd-3-505-2022
https://wcd.copernicus.org/articles/3/505/2022/
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spelling ftcopernicus:oai:publications.copernicus.org:wcd98537 2023-05-15T17:34:37+02:00 Quantifying climate model representation of the wintertime Euro-Atlantic circulation using geopotential-jet regimes Dorrington, Joshua Strommen, Kristian Fabiano, Federico 2022-04-20 application/pdf https://doi.org/10.5194/wcd-3-505-2022 https://wcd.copernicus.org/articles/3/505/2022/ eng eng doi:10.5194/wcd-3-505-2022 https://wcd.copernicus.org/articles/3/505/2022/ eISSN: 2698-4016 Text 2022 ftcopernicus https://doi.org/10.5194/wcd-3-505-2022 2022-04-25T16:22:30Z Even the most advanced climate models struggle to reproduce the observed wintertime circulation of the atmosphere over the North Atlantic and western Europe. During winter, the large-scale motions of this particularly challenging region are dominated by eddy-driven and highly non-linear flows, whose low-frequency variability is often studied from the perspective of regimes – a small number of qualitatively distinct atmospheric states. Poor representation of regimes associated with persistent atmospheric blocking events, or variations in jet latitude, degrades the ability of models to correctly simulate extreme events. In this paper we leverage a recently developed hybrid approach – which combines both jet and geopotential height data – to assess the representation of regimes in 8400 years of historical climate simulations drawn from the Coupled Model Intercomparison Project (CMIP) experiments, CMIP5, CMIP6, and HighResMIP. We show that these geopotential-jet regimes are particularly suited to the analysis of climate data, with considerable reductions in sampling variability compared to classical regime approaches. We find that CMIP6 has a considerably improved spatial regime structure, and a more trimodal eddy-driven jet, relative to CMIP5, but it still struggles with under-persistent regimes and too little European blocking when compared to reanalysis. Reduced regime persistence can be understood, at least in part, as a result of jets that are too fast and eddy feedbacks on the jet stream that are too weak – structural errors that do not noticeably improve in higher-resolution models. Text North Atlantic Copernicus Publications: E-Journals Weather and Climate Dynamics 3 2 505 533
institution Open Polar
collection Copernicus Publications: E-Journals
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language English
description Even the most advanced climate models struggle to reproduce the observed wintertime circulation of the atmosphere over the North Atlantic and western Europe. During winter, the large-scale motions of this particularly challenging region are dominated by eddy-driven and highly non-linear flows, whose low-frequency variability is often studied from the perspective of regimes – a small number of qualitatively distinct atmospheric states. Poor representation of regimes associated with persistent atmospheric blocking events, or variations in jet latitude, degrades the ability of models to correctly simulate extreme events. In this paper we leverage a recently developed hybrid approach – which combines both jet and geopotential height data – to assess the representation of regimes in 8400 years of historical climate simulations drawn from the Coupled Model Intercomparison Project (CMIP) experiments, CMIP5, CMIP6, and HighResMIP. We show that these geopotential-jet regimes are particularly suited to the analysis of climate data, with considerable reductions in sampling variability compared to classical regime approaches. We find that CMIP6 has a considerably improved spatial regime structure, and a more trimodal eddy-driven jet, relative to CMIP5, but it still struggles with under-persistent regimes and too little European blocking when compared to reanalysis. Reduced regime persistence can be understood, at least in part, as a result of jets that are too fast and eddy feedbacks on the jet stream that are too weak – structural errors that do not noticeably improve in higher-resolution models.
format Text
author Dorrington, Joshua
Strommen, Kristian
Fabiano, Federico
spellingShingle Dorrington, Joshua
Strommen, Kristian
Fabiano, Federico
Quantifying climate model representation of the wintertime Euro-Atlantic circulation using geopotential-jet regimes
author_facet Dorrington, Joshua
Strommen, Kristian
Fabiano, Federico
author_sort Dorrington, Joshua
title Quantifying climate model representation of the wintertime Euro-Atlantic circulation using geopotential-jet regimes
title_short Quantifying climate model representation of the wintertime Euro-Atlantic circulation using geopotential-jet regimes
title_full Quantifying climate model representation of the wintertime Euro-Atlantic circulation using geopotential-jet regimes
title_fullStr Quantifying climate model representation of the wintertime Euro-Atlantic circulation using geopotential-jet regimes
title_full_unstemmed Quantifying climate model representation of the wintertime Euro-Atlantic circulation using geopotential-jet regimes
title_sort quantifying climate model representation of the wintertime euro-atlantic circulation using geopotential-jet regimes
publishDate 2022
url https://doi.org/10.5194/wcd-3-505-2022
https://wcd.copernicus.org/articles/3/505/2022/
genre North Atlantic
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op_source eISSN: 2698-4016
op_relation doi:10.5194/wcd-3-505-2022
https://wcd.copernicus.org/articles/3/505/2022/
op_doi https://doi.org/10.5194/wcd-3-505-2022
container_title Weather and Climate Dynamics
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