A cold air cyclogenesis study using potential vorticity inversion method

A cold‐air cyclogenesis is studied using a potential vorticity (PV) inversion method. In this study, the method is coupled with the French spectral operational model ARPEGE which is initialized by four‐dimensional variational reanalyses. Sensitivity studies are performed for Intensive Observation Pe...

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Published in:Quarterly Journal of the Royal Meteorological Society
Main Authors: Lambert, Dominique, Arbogast, Philippe, Cammas, Jean-Pierre, Donnadille, Jérôme, Mascart, Patrick
Other Authors: Laboratoire d'aérologie (LAERO), Université Toulouse III - Paul Sabatier (UT3), Université de Toulouse (UT)-Université de Toulouse (UT)-Observatoire Midi-Pyrénées (OMP), Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Centre National de la Recherche Scientifique (CNRS), Centre national de recherches météorologiques (CNRM), Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Centre National de la Recherche Scientifique (CNRS)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2004
Subjects:
Online Access:https://hal.science/hal-00138153
https://hal.science/hal-00138153/document
https://hal.science/hal-00138153/file/Lambert2004.pdf
https://doi.org/10.1256/qj.03.37
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spelling ftmeteofrance:oai:HAL:hal-00138153v1 2024-09-15T18:12:39+00:00 A cold air cyclogenesis study using potential vorticity inversion method Lambert, Dominique Arbogast, Philippe Cammas, Jean-Pierre Donnadille, Jérôme Mascart, Patrick Laboratoire d'aérologie (LAERO) Université Toulouse III - Paul Sabatier (UT3) Université de Toulouse (UT)-Université de Toulouse (UT)-Observatoire Midi-Pyrénées (OMP) Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3) Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Centre National de la Recherche Scientifique (CNRS) Centre national de recherches météorologiques (CNRM) Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP) Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3) Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Centre National de la Recherche Scientifique (CNRS) 2004 https://hal.science/hal-00138153 https://hal.science/hal-00138153/document https://hal.science/hal-00138153/file/Lambert2004.pdf https://doi.org/10.1256/qj.03.37 en eng HAL CCSD Wiley info:eu-repo/semantics/altIdentifier/doi/10.1256/qj.03.37 hal-00138153 https://hal.science/hal-00138153 https://hal.science/hal-00138153/document https://hal.science/hal-00138153/file/Lambert2004.pdf doi:10.1256/qj.03.37 http://creativecommons.org/licenses/by/ info:eu-repo/semantics/OpenAccess ISSN: 0035-9009 EISSN: 1477-870X Quarterly Journal of the Royal Meteorological Society https://hal.science/hal-00138153 Quarterly Journal of the Royal Meteorological Society, 2004, 130 (603), pp.2953-2970. ⟨10.1256/qj.03.37⟩ ARPEGE model Fronts and Atlantic Storm-Track EXperiment Surface temperature [PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph] [SDU.STU.ME]Sciences of the Universe [physics]/Earth Sciences/Meteorology info:eu-repo/semantics/article Journal articles 2004 ftmeteofrance https://doi.org/10.1256/qj.03.37 2024-06-25T00:11:56Z A cold‐air cyclogenesis is studied using a potential vorticity (PV) inversion method. In this study, the method is coupled with the French spectral operational model ARPEGE which is initialized by four‐dimensional variational reanalyses. Sensitivity studies are performed for Intensive Observation Period 18 (IOP18) (low 44, 19–24 February 1997) of the Fronts and Atlantic Storm‐Track EXperiment (FASTEX). This event is one of the Type C cyclogeneses recently identified in the FASTEX dataset. The triggering role of a coherent tropopause disturbance on the cyclogenesis is discussed by comparing a reference forecast and a simulation in which the tropopause coherent structure is removed. Interactions between the atmospheric upper level and the cyclogenesis are found significant. A second important factor is the influence of the surface temperature. Evaluations of vertical motions for different surface temperature distributions show that the warmer the sea surface, the deeper the low. The location of the low with respect to the ice‐shelf limit is also an important factor. Article in Journal/Newspaper Ice Shelf Météo-France: HAL Quarterly Journal of the Royal Meteorological Society 130 603 2953 2970
institution Open Polar
collection Météo-France: HAL
op_collection_id ftmeteofrance
language English
topic ARPEGE model
Fronts and Atlantic Storm-Track EXperiment
Surface temperature
[PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph]
[SDU.STU.ME]Sciences of the Universe [physics]/Earth Sciences/Meteorology
spellingShingle ARPEGE model
Fronts and Atlantic Storm-Track EXperiment
Surface temperature
[PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph]
[SDU.STU.ME]Sciences of the Universe [physics]/Earth Sciences/Meteorology
Lambert, Dominique
Arbogast, Philippe
Cammas, Jean-Pierre
Donnadille, Jérôme
Mascart, Patrick
A cold air cyclogenesis study using potential vorticity inversion method
topic_facet ARPEGE model
Fronts and Atlantic Storm-Track EXperiment
Surface temperature
[PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph]
[SDU.STU.ME]Sciences of the Universe [physics]/Earth Sciences/Meteorology
description A cold‐air cyclogenesis is studied using a potential vorticity (PV) inversion method. In this study, the method is coupled with the French spectral operational model ARPEGE which is initialized by four‐dimensional variational reanalyses. Sensitivity studies are performed for Intensive Observation Period 18 (IOP18) (low 44, 19–24 February 1997) of the Fronts and Atlantic Storm‐Track EXperiment (FASTEX). This event is one of the Type C cyclogeneses recently identified in the FASTEX dataset. The triggering role of a coherent tropopause disturbance on the cyclogenesis is discussed by comparing a reference forecast and a simulation in which the tropopause coherent structure is removed. Interactions between the atmospheric upper level and the cyclogenesis are found significant. A second important factor is the influence of the surface temperature. Evaluations of vertical motions for different surface temperature distributions show that the warmer the sea surface, the deeper the low. The location of the low with respect to the ice‐shelf limit is also an important factor.
author2 Laboratoire d'aérologie (LAERO)
Université Toulouse III - Paul Sabatier (UT3)
Université de Toulouse (UT)-Université de Toulouse (UT)-Observatoire Midi-Pyrénées (OMP)
Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3)
Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Centre National de la Recherche Scientifique (CNRS)
Centre national de recherches météorologiques (CNRM)
Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP)
Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3)
Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Centre National de la Recherche Scientifique (CNRS)
format Article in Journal/Newspaper
author Lambert, Dominique
Arbogast, Philippe
Cammas, Jean-Pierre
Donnadille, Jérôme
Mascart, Patrick
author_facet Lambert, Dominique
Arbogast, Philippe
Cammas, Jean-Pierre
Donnadille, Jérôme
Mascart, Patrick
author_sort Lambert, Dominique
title A cold air cyclogenesis study using potential vorticity inversion method
title_short A cold air cyclogenesis study using potential vorticity inversion method
title_full A cold air cyclogenesis study using potential vorticity inversion method
title_fullStr A cold air cyclogenesis study using potential vorticity inversion method
title_full_unstemmed A cold air cyclogenesis study using potential vorticity inversion method
title_sort cold air cyclogenesis study using potential vorticity inversion method
publisher HAL CCSD
publishDate 2004
url https://hal.science/hal-00138153
https://hal.science/hal-00138153/document
https://hal.science/hal-00138153/file/Lambert2004.pdf
https://doi.org/10.1256/qj.03.37
genre Ice Shelf
genre_facet Ice Shelf
op_source ISSN: 0035-9009
EISSN: 1477-870X
Quarterly Journal of the Royal Meteorological Society
https://hal.science/hal-00138153
Quarterly Journal of the Royal Meteorological Society, 2004, 130 (603), pp.2953-2970. ⟨10.1256/qj.03.37⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1256/qj.03.37
hal-00138153
https://hal.science/hal-00138153
https://hal.science/hal-00138153/document
https://hal.science/hal-00138153/file/Lambert2004.pdf
doi:10.1256/qj.03.37
op_rights http://creativecommons.org/licenses/by/
info:eu-repo/semantics/OpenAccess
op_doi https://doi.org/10.1256/qj.03.37
container_title Quarterly Journal of the Royal Meteorological Society
container_volume 130
container_issue 603
container_start_page 2953
op_container_end_page 2970
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