Microphysics impacts on the warm conveyor belt and ridge building of the NAWDEX IOP6 cyclone

International audience This study investigates diabatic processes along the warm conveyor belt (WCB) of a deep extra-tropical cyclone observed of the North Atlantic Waveguide and Downstream Impact Experiment (NAWDEX). The aim is to investigate the effect of two different microphysics schemes, the on...

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Published in:Monthly Weather Review
Main Authors: Mazoyer, Marie, Ricard, Didier, Rivière, Gwendal, Delanoë, Julien, Arbogast, Philippe, Vié, Benoit, Lac, Christine, Cazenave, Quitterie, Pelon, Jacques
Other Authors: Centre national de recherches météorologiques (CNRM), Institut national des sciences de l'Univers (INSU - CNRS)-Météo France-Centre National de la Recherche Scientifique (CNRS), Laboratoire de Météorologie Dynamique (UMR 8539) (LMD), Institut national des sciences de l'Univers (INSU - CNRS)-École polytechnique (X)-École des Ponts ParisTech (ENPC)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-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), SPACE - LATMOS, Laboratoire Atmosphères, Milieux, Observations Spatiales (LATMOS), Sorbonne Université (SU)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2021
Subjects:
Online Access:https://hal-insu.archives-ouvertes.fr/insu-03381560
https://hal-insu.archives-ouvertes.fr/insu-03381560v2/document
https://hal-insu.archives-ouvertes.fr/insu-03381560v2/file/%255B15200493%2520-%2520Monthly%2520Weather%2520Review%255D%2520Microphysics%2520Impacts%2520on%2520the%2520Warm%2520Conveyor%2520Belt%2520and%2520Ridge%2520Building%2520of%2520the%2520NAWDEX%2520IOP6%2520Cyclone.pdf
https://doi.org/10.1175/MWR-D-21-0061.1
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institution Open Polar
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
Mazoyer, Marie
Ricard, Didier
Rivière, Gwendal
Delanoë, Julien
Arbogast, Philippe
Vié, Benoit
Lac, Christine
Cazenave, Quitterie
Pelon, Jacques
Microphysics impacts on the warm conveyor belt and ridge building of the NAWDEX IOP6 cyclone
topic_facet [SDU.STU.ME]Sciences of the Universe [physics]/Earth Sciences/Meteorology
description International audience This study investigates diabatic processes along the warm conveyor belt (WCB) of a deep extra-tropical cyclone observed of the North Atlantic Waveguide and Downstream Impact Experiment (NAWDEX). The aim is to investigate the effect of two different microphysics schemes, the one-moment scheme ICE3 and the quasi two-moment scheme LIMA, on the WCB and the ridge building downstream. ICE3 and LIMA also differ on the processes of vapor deposition on hydrometeors in cold and mixed-phase clouds. Latent heating in ICE3 is found to be dominated by deposition on ice while the heating in LIMA is distributed among depositions on ice, snow and graupel. ICE3 is the scheme leading to the largest number of WCB trajectories (30% more than LIMA) due to greater heating rates over larger areas. The consequence is that the size of the upper-level ridge is growing more rapidly in ICE3 than LIMA, albeit with some exceptions in localized regions of the cyclonic branch of the WCB. A comparison with various observations (airborne remote sensing measurements, dropsondes and satellite data) is then performed. Below the melting layer, the observed reflectivity is rather well reproduced by the model. Above the melting layer, in the middle of the troposphere, the reflectivity and retrieved ice water content are largely underestimated by both schemes while at upper levels, the ICE3 scheme performs much better than LIMA in agreement with a closer representation of the observed winds by ICE3. These results underline the strong sensitivity of upper-level dynamics to ice related processes.
author2 Centre national de recherches météorologiques (CNRM)
Institut national des sciences de l'Univers (INSU - CNRS)-Météo France-Centre National de la Recherche Scientifique (CNRS)
Laboratoire de Météorologie Dynamique (UMR 8539) (LMD)
Institut national des sciences de l'Univers (INSU - CNRS)-École polytechnique (X)-École des Ponts ParisTech (ENPC)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-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)
SPACE - LATMOS
Laboratoire Atmosphères, Milieux, Observations Spatiales (LATMOS)
Sorbonne Université (SU)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)
format Article in Journal/Newspaper
author Mazoyer, Marie
Ricard, Didier
Rivière, Gwendal
Delanoë, Julien
Arbogast, Philippe
Vié, Benoit
Lac, Christine
Cazenave, Quitterie
Pelon, Jacques
author_facet Mazoyer, Marie
Ricard, Didier
Rivière, Gwendal
Delanoë, Julien
Arbogast, Philippe
Vié, Benoit
Lac, Christine
Cazenave, Quitterie
Pelon, Jacques
author_sort Mazoyer, Marie
title Microphysics impacts on the warm conveyor belt and ridge building of the NAWDEX IOP6 cyclone
title_short Microphysics impacts on the warm conveyor belt and ridge building of the NAWDEX IOP6 cyclone
title_full Microphysics impacts on the warm conveyor belt and ridge building of the NAWDEX IOP6 cyclone
title_fullStr Microphysics impacts on the warm conveyor belt and ridge building of the NAWDEX IOP6 cyclone
title_full_unstemmed Microphysics impacts on the warm conveyor belt and ridge building of the NAWDEX IOP6 cyclone
title_sort microphysics impacts on the warm conveyor belt and ridge building of the nawdex iop6 cyclone
publisher HAL CCSD
publishDate 2021
url https://hal-insu.archives-ouvertes.fr/insu-03381560
https://hal-insu.archives-ouvertes.fr/insu-03381560v2/document
https://hal-insu.archives-ouvertes.fr/insu-03381560v2/file/%255B15200493%2520-%2520Monthly%2520Weather%2520Review%255D%2520Microphysics%2520Impacts%2520on%2520the%2520Warm%2520Conveyor%2520Belt%2520and%2520Ridge%2520Building%2520of%2520the%2520NAWDEX%2520IOP6%2520Cyclone.pdf
https://doi.org/10.1175/MWR-D-21-0061.1
genre North Atlantic
genre_facet North Atlantic
op_source ISSN: 0027-0644
EISSN: 1520-0493
Monthly Weather Review
https://hal-insu.archives-ouvertes.fr/insu-03381560
Monthly Weather Review, American Meteorological Society, 2021, 149 (12), pp.3961-3980. ⟨10.1175/MWR-D-21-0061.1⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1175/MWR-D-21-0061.1
insu-03381560
https://hal-insu.archives-ouvertes.fr/insu-03381560
https://hal-insu.archives-ouvertes.fr/insu-03381560v2/document
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doi:10.1175/MWR-D-21-0061.1
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container_title Monthly Weather Review
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spelling ftccsdartic:oai:HAL:insu-03381560v2 2023-05-15T17:35:11+02:00 Microphysics impacts on the warm conveyor belt and ridge building of the NAWDEX IOP6 cyclone Mazoyer, Marie Ricard, Didier Rivière, Gwendal Delanoë, Julien Arbogast, Philippe Vié, Benoit Lac, Christine Cazenave, Quitterie Pelon, Jacques Centre national de recherches météorologiques (CNRM) Institut national des sciences de l'Univers (INSU - CNRS)-Météo France-Centre National de la Recherche Scientifique (CNRS) Laboratoire de Météorologie Dynamique (UMR 8539) (LMD) Institut national des sciences de l'Univers (INSU - CNRS)-École polytechnique (X)-École des Ponts ParisTech (ENPC)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-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) SPACE - LATMOS Laboratoire Atmosphères, Milieux, Observations Spatiales (LATMOS) Sorbonne Université (SU)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS) 2021-10-13 https://hal-insu.archives-ouvertes.fr/insu-03381560 https://hal-insu.archives-ouvertes.fr/insu-03381560v2/document https://hal-insu.archives-ouvertes.fr/insu-03381560v2/file/%255B15200493%2520-%2520Monthly%2520Weather%2520Review%255D%2520Microphysics%2520Impacts%2520on%2520the%2520Warm%2520Conveyor%2520Belt%2520and%2520Ridge%2520Building%2520of%2520the%2520NAWDEX%2520IOP6%2520Cyclone.pdf https://doi.org/10.1175/MWR-D-21-0061.1 en eng HAL CCSD American Meteorological Society info:eu-repo/semantics/altIdentifier/doi/10.1175/MWR-D-21-0061.1 insu-03381560 https://hal-insu.archives-ouvertes.fr/insu-03381560 https://hal-insu.archives-ouvertes.fr/insu-03381560v2/document https://hal-insu.archives-ouvertes.fr/insu-03381560v2/file/%255B15200493%2520-%2520Monthly%2520Weather%2520Review%255D%2520Microphysics%2520Impacts%2520on%2520the%2520Warm%2520Conveyor%2520Belt%2520and%2520Ridge%2520Building%2520of%2520the%2520NAWDEX%2520IOP6%2520Cyclone.pdf doi:10.1175/MWR-D-21-0061.1 http://creativecommons.org/licenses/by/ info:eu-repo/semantics/OpenAccess ISSN: 0027-0644 EISSN: 1520-0493 Monthly Weather Review https://hal-insu.archives-ouvertes.fr/insu-03381560 Monthly Weather Review, American Meteorological Society, 2021, 149 (12), pp.3961-3980. ⟨10.1175/MWR-D-21-0061.1⟩ [SDU.STU.ME]Sciences of the Universe [physics]/Earth Sciences/Meteorology info:eu-repo/semantics/article Journal articles 2021 ftccsdartic https://doi.org/10.1175/MWR-D-21-0061.1 2022-01-08T23:42:11Z International audience This study investigates diabatic processes along the warm conveyor belt (WCB) of a deep extra-tropical cyclone observed of the North Atlantic Waveguide and Downstream Impact Experiment (NAWDEX). The aim is to investigate the effect of two different microphysics schemes, the one-moment scheme ICE3 and the quasi two-moment scheme LIMA, on the WCB and the ridge building downstream. ICE3 and LIMA also differ on the processes of vapor deposition on hydrometeors in cold and mixed-phase clouds. Latent heating in ICE3 is found to be dominated by deposition on ice while the heating in LIMA is distributed among depositions on ice, snow and graupel. ICE3 is the scheme leading to the largest number of WCB trajectories (30% more than LIMA) due to greater heating rates over larger areas. The consequence is that the size of the upper-level ridge is growing more rapidly in ICE3 than LIMA, albeit with some exceptions in localized regions of the cyclonic branch of the WCB. A comparison with various observations (airborne remote sensing measurements, dropsondes and satellite data) is then performed. Below the melting layer, the observed reflectivity is rather well reproduced by the model. Above the melting layer, in the middle of the troposphere, the reflectivity and retrieved ice water content are largely underestimated by both schemes while at upper levels, the ICE3 scheme performs much better than LIMA in agreement with a closer representation of the observed winds by ICE3. These results underline the strong sensitivity of upper-level dynamics to ice related processes. Article in Journal/Newspaper North Atlantic Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) Monthly Weather Review 149 12 3961 3980