Influence of Arctic Sea ice concentration on extended-range prediction of strong and Long-lasting ural blocking events in Winter

It is traditionally considered that the predictability of atmosphere reaches approximately 2 weeks due to its chaotic features. Considering boundary conditions, the lead prediction time can exceed 2 weeks in certain cases. We find that the Arctic sea ice concentration (SIC) is crucial for extended-r...

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Main Authors: Mu, M., Dai, G., Ma, X.
Format: Conference Object
Language:English
Published: 2023
Subjects:
Online Access:https://gfzpublic.gfz-potsdam.de/pubman/item/item_5016779
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spelling ftgfzpotsdam:oai:gfzpublic.gfz-potsdam.de:item_5016779 2023-06-11T04:09:12+02:00 Influence of Arctic Sea ice concentration on extended-range prediction of strong and Long-lasting ural blocking events in Winter Mu, M. Dai, G. Ma, X. 2023 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5016779 eng eng info:eu-repo/semantics/altIdentifier/doi/10.57757/IUGG23-0708 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5016779 XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG) info:eu-repo/semantics/conferenceObject 2023 ftgfzpotsdam https://doi.org/10.57757/IUGG23-0708 2023-05-07T23:38:37Z It is traditionally considered that the predictability of atmosphere reaches approximately 2 weeks due to its chaotic features. Considering boundary conditions, the lead prediction time can exceed 2 weeks in certain cases. We find that the Arctic sea ice concentration (SIC) is crucial for extended-range prediction of strong and long-lasting Ural blocking (UB) formation. By applying the rotated empirical orthogonal function-based particle swarm optimization algorithm, the conditional nonlinear optimal perturbation is calculated with the Community Atmosphere Model, version 4, to identify the optimally growing boundary errors in extended-range prediction of strong and long-lasting UB formation. It is found that SIC perturbations in the Greenland Sea (GS), Barents Sea (BS), and Okhotsk Sea (OKS) are important for strong and long-lasting UB formation prediction in four pentads. Further analysis reveals that the SIC perturbations in these areas first influence the local temperature field through the diabatic heating process and further affect the temperature field in the Ural sector mainly by advection and convection processes. Moreover, the zonal winds in the Ural sector are adjusted by the thermal wind balance, thus affecting UB formation. The local characteristics of the SIC perturbations indicate that the GS, BS, and OKS may be sensitive areas in regard to extended-range prediction of strong and long-lasting UB formation, which can provide scientific support for the SIC target observations in the future. Conference Object Arctic Barents Sea Greenland Greenland Sea okhotsk sea Sea ice GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam) Arctic Barents Sea Greenland Okhotsk
institution Open Polar
collection GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam)
op_collection_id ftgfzpotsdam
language English
description It is traditionally considered that the predictability of atmosphere reaches approximately 2 weeks due to its chaotic features. Considering boundary conditions, the lead prediction time can exceed 2 weeks in certain cases. We find that the Arctic sea ice concentration (SIC) is crucial for extended-range prediction of strong and long-lasting Ural blocking (UB) formation. By applying the rotated empirical orthogonal function-based particle swarm optimization algorithm, the conditional nonlinear optimal perturbation is calculated with the Community Atmosphere Model, version 4, to identify the optimally growing boundary errors in extended-range prediction of strong and long-lasting UB formation. It is found that SIC perturbations in the Greenland Sea (GS), Barents Sea (BS), and Okhotsk Sea (OKS) are important for strong and long-lasting UB formation prediction in four pentads. Further analysis reveals that the SIC perturbations in these areas first influence the local temperature field through the diabatic heating process and further affect the temperature field in the Ural sector mainly by advection and convection processes. Moreover, the zonal winds in the Ural sector are adjusted by the thermal wind balance, thus affecting UB formation. The local characteristics of the SIC perturbations indicate that the GS, BS, and OKS may be sensitive areas in regard to extended-range prediction of strong and long-lasting UB formation, which can provide scientific support for the SIC target observations in the future.
format Conference Object
author Mu, M.
Dai, G.
Ma, X.
spellingShingle Mu, M.
Dai, G.
Ma, X.
Influence of Arctic Sea ice concentration on extended-range prediction of strong and Long-lasting ural blocking events in Winter
author_facet Mu, M.
Dai, G.
Ma, X.
author_sort Mu, M.
title Influence of Arctic Sea ice concentration on extended-range prediction of strong and Long-lasting ural blocking events in Winter
title_short Influence of Arctic Sea ice concentration on extended-range prediction of strong and Long-lasting ural blocking events in Winter
title_full Influence of Arctic Sea ice concentration on extended-range prediction of strong and Long-lasting ural blocking events in Winter
title_fullStr Influence of Arctic Sea ice concentration on extended-range prediction of strong and Long-lasting ural blocking events in Winter
title_full_unstemmed Influence of Arctic Sea ice concentration on extended-range prediction of strong and Long-lasting ural blocking events in Winter
title_sort influence of arctic sea ice concentration on extended-range prediction of strong and long-lasting ural blocking events in winter
publishDate 2023
url https://gfzpublic.gfz-potsdam.de/pubman/item/item_5016779
geographic Arctic
Barents Sea
Greenland
Okhotsk
geographic_facet Arctic
Barents Sea
Greenland
Okhotsk
genre Arctic
Barents Sea
Greenland
Greenland Sea
okhotsk sea
Sea ice
genre_facet Arctic
Barents Sea
Greenland
Greenland Sea
okhotsk sea
Sea ice
op_source XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG)
op_relation info:eu-repo/semantics/altIdentifier/doi/10.57757/IUGG23-0708
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5016779
op_doi https://doi.org/10.57757/IUGG23-0708
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