Polar lows over the Nordic seas: Improved representation in ERA-interim compared to ERA-40 and the impact on downscaled simulations

International audience Polar lows are intense high-latitude mesocyclones that form during the cold season over open sea. Their relatively small-scale and short life span lead to a rather poor representation in model outputs and meteorological reanalyses. In this paper, the ability of the Interim Eur...

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Published in:Monthly Weather Review
Main Authors: Laffineur, Thibaud, Claud, Chantal, Chaboureau, Jean-Pierre, Noer, G.
Other Authors: Ecole Nationale de la Météorologie, Institut National Polytechnique (Toulouse) (Toulouse INP), Université Fédérale Toulouse Midi-Pyrénées-Université Fédérale Toulouse Midi-Pyrénées, Laboratoire de Météorologie Dynamique (UMR 8539) (LMD), Département des Géosciences - ENS Paris, École normale supérieure - Paris (ENS Paris), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-École normale supérieure - Paris (ENS Paris), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Centre National de la Recherche Scientifique (CNRS)-École des Ponts ParisTech (ENPC)-École polytechnique (X)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Pierre et Marie Curie - Paris 6 (UPMC), Laboratoire d'aérologie (LAERO), Centre National de la Recherche Scientifique (CNRS)-Observatoire Midi-Pyrénées (OMP), Météo France-Centre National d'Études Spatiales Toulouse (CNES)-Université Fédérale Toulouse Midi-Pyrénées-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Météo France-Centre National d'Études Spatiales Toulouse (CNES)-Université Fédérale Toulouse Midi-Pyrénées-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3), Université Fédérale Toulouse Midi-Pyrénées, Norwegian Meteorological Institute Oslo (MET)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2014
Subjects:
Online Access:https://hal.archives-ouvertes.fr/hal-01087286
https://hal.archives-ouvertes.fr/hal-01087286/document
https://hal.archives-ouvertes.fr/hal-01087286/file/%5B15200493%20-%20Monthly%20Weather%20Review%5D%20Polar%20Lows%20over%20the%20Nordic%20Seas%20Improved%20Representation%20in%20ERA-Interim%20Compared%20to%20ERA-40%20and%20the%20Impact%20on%20Downscaled%20Simulations.pdf
https://doi.org/10.1175/MWR-D-13-00171.1
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collection Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe)
op_collection_id ftccsdartic
language English
topic [SDU.STU.ME]Sciences of the Universe [physics]/Earth Sciences/Meteorology
spellingShingle [SDU.STU.ME]Sciences of the Universe [physics]/Earth Sciences/Meteorology
Laffineur, Thibaud
Claud, Chantal
Chaboureau, Jean-Pierre
Noer, G.
Polar lows over the Nordic seas: Improved representation in ERA-interim compared to ERA-40 and the impact on downscaled simulations
topic_facet [SDU.STU.ME]Sciences of the Universe [physics]/Earth Sciences/Meteorology
description International audience Polar lows are intense high-latitude mesocyclones that form during the cold season over open sea. Their relatively small-scale and short life span lead to a rather poor representation in model outputs and meteorological reanalyses. In this paper, the ability of the Interim European Centre for Medium-Range Weather Forecasts (ECMWF) Re-Analysis (ERA-Interim) to represent polar lows over the Norwegian and Barents Sea is assessed, and a comparison with the 40-yr ECMWF Re-Analysis (ERA-40) is provided for three cold seasons (1999-2000 until 2001-02). A better representation in ERA-Interim is found, with 13 systems captured out of the 29 observed, against 6 in the case of ERA-40. Reasons for the lack of representation are identified. Unexpectedly, the representation of different polar low sizes does not appear to be linked to the resolution. Rather, it is the representation of synoptic conditions that appears to be essential. In a second part, a downscaling is conducted using the mesoscale model Méso-NH. For each observed polar low, a pair of simulations is performed: one initialized by ERA-Interim and the other one by ERA-40. An improvement is noted with 22 polar lows represented when ERA-Interim is used. Through a model-to-satellite approach, it is shown that even if polar lows are simulated, convective processes remain insufficiently represented. Wind speeds, which were underestimated in reanalyses, are nevertheless more realistic in the Méso-NH simulations. These results are supported by a spectral analysis of reanalyses and Méso-NH fields. © 2014 American Meteorological Society.
author2 Ecole Nationale de la Météorologie
Institut National Polytechnique (Toulouse) (Toulouse INP)
Université Fédérale Toulouse Midi-Pyrénées-Université Fédérale Toulouse Midi-Pyrénées
Laboratoire de Météorologie Dynamique (UMR 8539) (LMD)
Département des Géosciences - ENS Paris
École normale supérieure - Paris (ENS Paris)
Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-École normale supérieure - Paris (ENS Paris)
Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Centre National de la Recherche Scientifique (CNRS)-École des Ponts ParisTech (ENPC)-École polytechnique (X)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Pierre et Marie Curie - Paris 6 (UPMC)
Laboratoire d'aérologie (LAERO)
Centre National de la Recherche Scientifique (CNRS)-Observatoire Midi-Pyrénées (OMP)
Météo France-Centre National d'Études Spatiales Toulouse (CNES)-Université Fédérale Toulouse Midi-Pyrénées-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Météo France-Centre National d'Études Spatiales Toulouse (CNES)-Université Fédérale Toulouse Midi-Pyrénées-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3)
Université Fédérale Toulouse Midi-Pyrénées
Norwegian Meteorological Institute Oslo (MET)
format Article in Journal/Newspaper
author Laffineur, Thibaud
Claud, Chantal
Chaboureau, Jean-Pierre
Noer, G.
author_facet Laffineur, Thibaud
Claud, Chantal
Chaboureau, Jean-Pierre
Noer, G.
author_sort Laffineur, Thibaud
title Polar lows over the Nordic seas: Improved representation in ERA-interim compared to ERA-40 and the impact on downscaled simulations
title_short Polar lows over the Nordic seas: Improved representation in ERA-interim compared to ERA-40 and the impact on downscaled simulations
title_full Polar lows over the Nordic seas: Improved representation in ERA-interim compared to ERA-40 and the impact on downscaled simulations
title_fullStr Polar lows over the Nordic seas: Improved representation in ERA-interim compared to ERA-40 and the impact on downscaled simulations
title_full_unstemmed Polar lows over the Nordic seas: Improved representation in ERA-interim compared to ERA-40 and the impact on downscaled simulations
title_sort polar lows over the nordic seas: improved representation in era-interim compared to era-40 and the impact on downscaled simulations
publisher HAL CCSD
publishDate 2014
url https://hal.archives-ouvertes.fr/hal-01087286
https://hal.archives-ouvertes.fr/hal-01087286/document
https://hal.archives-ouvertes.fr/hal-01087286/file/%5B15200493%20-%20Monthly%20Weather%20Review%5D%20Polar%20Lows%20over%20the%20Nordic%20Seas%20Improved%20Representation%20in%20ERA-Interim%20Compared%20to%20ERA-40%20and%20the%20Impact%20on%20Downscaled%20Simulations.pdf
https://doi.org/10.1175/MWR-D-13-00171.1
geographic Barents Sea
geographic_facet Barents Sea
genre Barents Sea
Nordic Seas
genre_facet Barents Sea
Nordic Seas
op_source ISSN: 0027-0644
EISSN: 1520-0493
Monthly Weather Review
https://hal.archives-ouvertes.fr/hal-01087286
Monthly Weather Review, American Meteorological Society, 2014, 142 (6), pp.2271-2289. ⟨10.1175/MWR-D-13-00171.1⟩
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hal-01087286
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doi:10.1175/MWR-D-13-00171.1
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spelling ftccsdartic:oai:HAL:hal-01087286v1 2023-05-15T15:39:07+02:00 Polar lows over the Nordic seas: Improved representation in ERA-interim compared to ERA-40 and the impact on downscaled simulations Laffineur, Thibaud Claud, Chantal Chaboureau, Jean-Pierre Noer, G. Ecole Nationale de la Météorologie Institut National Polytechnique (Toulouse) (Toulouse INP) Université Fédérale Toulouse Midi-Pyrénées-Université Fédérale Toulouse Midi-Pyrénées Laboratoire de Météorologie Dynamique (UMR 8539) (LMD) Département des Géosciences - ENS Paris École normale supérieure - Paris (ENS Paris) Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-École normale supérieure - Paris (ENS Paris) Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Centre National de la Recherche Scientifique (CNRS)-École des Ponts ParisTech (ENPC)-École polytechnique (X)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Pierre et Marie Curie - Paris 6 (UPMC) Laboratoire d'aérologie (LAERO) Centre National de la Recherche Scientifique (CNRS)-Observatoire Midi-Pyrénées (OMP) Météo France-Centre National d'Études Spatiales Toulouse (CNES)-Université Fédérale Toulouse Midi-Pyrénées-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Météo France-Centre National d'Études Spatiales Toulouse (CNES)-Université Fédérale Toulouse Midi-Pyrénées-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3) Université Fédérale Toulouse Midi-Pyrénées Norwegian Meteorological Institute Oslo (MET) 2014 https://hal.archives-ouvertes.fr/hal-01087286 https://hal.archives-ouvertes.fr/hal-01087286/document https://hal.archives-ouvertes.fr/hal-01087286/file/%5B15200493%20-%20Monthly%20Weather%20Review%5D%20Polar%20Lows%20over%20the%20Nordic%20Seas%20Improved%20Representation%20in%20ERA-Interim%20Compared%20to%20ERA-40%20and%20the%20Impact%20on%20Downscaled%20Simulations.pdf https://doi.org/10.1175/MWR-D-13-00171.1 en eng HAL CCSD American Meteorological Society info:eu-repo/semantics/altIdentifier/doi/10.1175/MWR-D-13-00171.1 hal-01087286 https://hal.archives-ouvertes.fr/hal-01087286 https://hal.archives-ouvertes.fr/hal-01087286/document https://hal.archives-ouvertes.fr/hal-01087286/file/%5B15200493%20-%20Monthly%20Weather%20Review%5D%20Polar%20Lows%20over%20the%20Nordic%20Seas%20Improved%20Representation%20in%20ERA-Interim%20Compared%20to%20ERA-40%20and%20the%20Impact%20on%20Downscaled%20Simulations.pdf doi:10.1175/MWR-D-13-00171.1 http://creativecommons.org/licenses/by/ info:eu-repo/semantics/OpenAccess ISSN: 0027-0644 EISSN: 1520-0493 Monthly Weather Review https://hal.archives-ouvertes.fr/hal-01087286 Monthly Weather Review, American Meteorological Society, 2014, 142 (6), pp.2271-2289. ⟨10.1175/MWR-D-13-00171.1⟩ [SDU.STU.ME]Sciences of the Universe [physics]/Earth Sciences/Meteorology info:eu-repo/semantics/article Journal articles 2014 ftccsdartic https://doi.org/10.1175/MWR-D-13-00171.1 2021-12-25T23:30:59Z International audience Polar lows are intense high-latitude mesocyclones that form during the cold season over open sea. Their relatively small-scale and short life span lead to a rather poor representation in model outputs and meteorological reanalyses. In this paper, the ability of the Interim European Centre for Medium-Range Weather Forecasts (ECMWF) Re-Analysis (ERA-Interim) to represent polar lows over the Norwegian and Barents Sea is assessed, and a comparison with the 40-yr ECMWF Re-Analysis (ERA-40) is provided for three cold seasons (1999-2000 until 2001-02). A better representation in ERA-Interim is found, with 13 systems captured out of the 29 observed, against 6 in the case of ERA-40. Reasons for the lack of representation are identified. Unexpectedly, the representation of different polar low sizes does not appear to be linked to the resolution. Rather, it is the representation of synoptic conditions that appears to be essential. In a second part, a downscaling is conducted using the mesoscale model Méso-NH. For each observed polar low, a pair of simulations is performed: one initialized by ERA-Interim and the other one by ERA-40. An improvement is noted with 22 polar lows represented when ERA-Interim is used. Through a model-to-satellite approach, it is shown that even if polar lows are simulated, convective processes remain insufficiently represented. Wind speeds, which were underestimated in reanalyses, are nevertheless more realistic in the Méso-NH simulations. These results are supported by a spectral analysis of reanalyses and Méso-NH fields. © 2014 American Meteorological Society. Article in Journal/Newspaper Barents Sea Nordic Seas Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) Barents Sea Monthly Weather Review 142 6 2271 2289