Intermittent African Easterly Wave Activity in a Dry Atmospheric Model: Influence of the Extratropics

International audience A dynamical model is constructed of the northern summertime global circulation, maintained by empirically derived forcing, based on the same dynamical code that has recently been used to study African easterly waves (AEWs) as convectively triggered perturbations (Thorncroft et...

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Published in:Journal of Climate
Main Authors: Leroux, Stephanie, Hall, Nicholas M. J., Kiladis, George N.
Other Authors: National Oceanic and Atmospheric Administration (NOAA), Océan du Large et Variabilité Climatique (OLVAC), Laboratoire d'études en Géophysique et océanographie spatiales (LEGOS), Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3), Université Fédérale Toulouse Midi-Pyrénées-Université Fédérale Toulouse Midi-Pyrénées-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP), Université Fédérale Toulouse Midi-Pyrénées-Université Fédérale Toulouse Midi-Pyrénées-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)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -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-Université Fédérale Toulouse Midi-Pyrénées-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)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Centre National de la Recherche Scientifique (CNRS), NOAA Earth System Research Laboratory (ESRL)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2011
Subjects:
Online Access:https://hal.science/hal-00798734
https://hal.science/hal-00798734/document
https://hal.science/hal-00798734/file/jcli-d-11-00049_2E1.pdf
https://doi.org/10.1175/JCLI-D-11-00049.1
id ftunivnantes:oai:HAL:hal-00798734v1
record_format openpolar
institution Open Polar
collection Université de Nantes: HAL-UNIV-NANTES
op_collection_id ftunivnantes
language English
topic Africa
Tropics
Waves
atmospheric
Monsoons
Summer/warm season
Synoptic-scale processes
General circulation models
[SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
spellingShingle Africa
Tropics
Waves
atmospheric
Monsoons
Summer/warm season
Synoptic-scale processes
General circulation models
[SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
Leroux, Stephanie
Hall, Nicholas M. J.
Kiladis, George N.
Intermittent African Easterly Wave Activity in a Dry Atmospheric Model: Influence of the Extratropics
topic_facet Africa
Tropics
Waves
atmospheric
Monsoons
Summer/warm season
Synoptic-scale processes
General circulation models
[SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
description International audience A dynamical model is constructed of the northern summertime global circulation, maintained by empirically derived forcing, based on the same dynamical code that has recently been used to study African easterly waves (AEWs) as convectively triggered perturbations (Thorncroft et al.; Leroux and Hall). In the configuration used here, the model faithfully simulates the observed mean distributions of jets and transient disturbances, and explicitly represents the interactions between them. This simple GCM is used to investigate the origin and intraseasonal intermittency of AEWs in an artificially dry (no convection) context. A long integration of the model produces a summertime climatology that includes a realistic African easterly jet and westward-propagating 3-5-day disturbances over West Africa. These simulated waves display intraseasonal intermittency as the observed AEWs also do. Further experiments designed to discern the source of this intermittency in the model show that the simulated waves are mainly triggered by dynamical precursors coming from the North Atlantic storm track. The model is at least as sensitive to this remote influence as it is to local triggering by convective heating.
author2 National Oceanic and Atmospheric Administration (NOAA)
Océan du Large et Variabilité Climatique (OLVAC)
Laboratoire d'études en Géophysique et océanographie spatiales (LEGOS)
Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3)
Université Fédérale Toulouse Midi-Pyrénées-Université Fédérale Toulouse Midi-Pyrénées-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP)
Université Fédérale Toulouse Midi-Pyrénées-Université Fédérale Toulouse Midi-Pyrénées-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)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -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-Université Fédérale Toulouse Midi-Pyrénées-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)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Centre National de la Recherche Scientifique (CNRS)
NOAA Earth System Research Laboratory (ESRL)
format Article in Journal/Newspaper
author Leroux, Stephanie
Hall, Nicholas M. J.
Kiladis, George N.
author_facet Leroux, Stephanie
Hall, Nicholas M. J.
Kiladis, George N.
author_sort Leroux, Stephanie
title Intermittent African Easterly Wave Activity in a Dry Atmospheric Model: Influence of the Extratropics
title_short Intermittent African Easterly Wave Activity in a Dry Atmospheric Model: Influence of the Extratropics
title_full Intermittent African Easterly Wave Activity in a Dry Atmospheric Model: Influence of the Extratropics
title_fullStr Intermittent African Easterly Wave Activity in a Dry Atmospheric Model: Influence of the Extratropics
title_full_unstemmed Intermittent African Easterly Wave Activity in a Dry Atmospheric Model: Influence of the Extratropics
title_sort intermittent african easterly wave activity in a dry atmospheric model: influence of the extratropics
publisher HAL CCSD
publishDate 2011
url https://hal.science/hal-00798734
https://hal.science/hal-00798734/document
https://hal.science/hal-00798734/file/jcli-d-11-00049_2E1.pdf
https://doi.org/10.1175/JCLI-D-11-00049.1
long_lat ENVELOPE(-64.231,-64.231,-65.619,-65.619)
geographic Leroux
geographic_facet Leroux
genre North Atlantic
genre_facet North Atlantic
op_source ISSN: 0894-8755
EISSN: 1520-0442
Journal of Climate
https://hal.science/hal-00798734
Journal of Climate, 2011, 24, pp.5378-5396. ⟨10.1175/JCLI-D-11-00049.1⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1175/JCLI-D-11-00049.1
hal-00798734
https://hal.science/hal-00798734
https://hal.science/hal-00798734/document
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doi:10.1175/JCLI-D-11-00049.1
op_rights info:eu-repo/semantics/OpenAccess
op_doi https://doi.org/10.1175/JCLI-D-11-00049.1
container_title Journal of Climate
container_volume 24
container_issue 20
container_start_page 5378
op_container_end_page 5396
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spelling ftunivnantes:oai:HAL:hal-00798734v1 2023-05-15T17:33:51+02:00 Intermittent African Easterly Wave Activity in a Dry Atmospheric Model: Influence of the Extratropics Leroux, Stephanie Hall, Nicholas M. J. Kiladis, George N. National Oceanic and Atmospheric Administration (NOAA) Océan du Large et Variabilité Climatique (OLVAC) Laboratoire d'études en Géophysique et océanographie spatiales (LEGOS) Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3) Université Fédérale Toulouse Midi-Pyrénées-Université Fédérale Toulouse Midi-Pyrénées-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP) Université Fédérale Toulouse Midi-Pyrénées-Université Fédérale Toulouse Midi-Pyrénées-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)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -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-Université Fédérale Toulouse Midi-Pyrénées-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)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Centre National de la Recherche Scientifique (CNRS) NOAA Earth System Research Laboratory (ESRL) 2011-10 https://hal.science/hal-00798734 https://hal.science/hal-00798734/document https://hal.science/hal-00798734/file/jcli-d-11-00049_2E1.pdf https://doi.org/10.1175/JCLI-D-11-00049.1 en eng HAL CCSD American Meteorological Society info:eu-repo/semantics/altIdentifier/doi/10.1175/JCLI-D-11-00049.1 hal-00798734 https://hal.science/hal-00798734 https://hal.science/hal-00798734/document https://hal.science/hal-00798734/file/jcli-d-11-00049_2E1.pdf doi:10.1175/JCLI-D-11-00049.1 info:eu-repo/semantics/OpenAccess ISSN: 0894-8755 EISSN: 1520-0442 Journal of Climate https://hal.science/hal-00798734 Journal of Climate, 2011, 24, pp.5378-5396. ⟨10.1175/JCLI-D-11-00049.1⟩ Africa Tropics Waves atmospheric Monsoons Summer/warm season Synoptic-scale processes General circulation models [SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere info:eu-repo/semantics/article Journal articles 2011 ftunivnantes https://doi.org/10.1175/JCLI-D-11-00049.1 2023-02-22T00:03:47Z International audience A dynamical model is constructed of the northern summertime global circulation, maintained by empirically derived forcing, based on the same dynamical code that has recently been used to study African easterly waves (AEWs) as convectively triggered perturbations (Thorncroft et al.; Leroux and Hall). In the configuration used here, the model faithfully simulates the observed mean distributions of jets and transient disturbances, and explicitly represents the interactions between them. This simple GCM is used to investigate the origin and intraseasonal intermittency of AEWs in an artificially dry (no convection) context. A long integration of the model produces a summertime climatology that includes a realistic African easterly jet and westward-propagating 3-5-day disturbances over West Africa. These simulated waves display intraseasonal intermittency as the observed AEWs also do. Further experiments designed to discern the source of this intermittency in the model show that the simulated waves are mainly triggered by dynamical precursors coming from the North Atlantic storm track. The model is at least as sensitive to this remote influence as it is to local triggering by convective heating. Article in Journal/Newspaper North Atlantic Université de Nantes: HAL-UNIV-NANTES Leroux ENVELOPE(-64.231,-64.231,-65.619,-65.619) Journal of Climate 24 20 5378 5396