New Insights into the Vertical Structure of Clouds in Polar Lows, using Radar‐Lidar Satellite Observations

International audience For the first time, we characterize the vertical distribution of cloud microphysical properties in polar lows (PLs). We base our investigation on colocations found between A-Train satellites overpasses and 82 PL occurrences evidenced from AVHRR observations in the Nordic Seas....

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Published in:Geophysical Research Letters
Main Authors: Listowski, Constantino, Rojo, Mathias, Claud, Chantal, Delanoë, Julien, Rysman, Jean-François, Cazenave, Quitterie, Noer, G.
Other Authors: Laboratoire Atmosphères, Milieux, Observations Spatiales (LATMOS), Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS), DAM Île-de-France (DAM/DIF), Direction des Applications Militaires (DAM), Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA), 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-PSL), Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-École normale supérieure - Paris (ENS-PSL), Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL), SPACE - LATMOS, Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS), Norwegian Meteorological Institute Oslo (MET)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2020
Subjects:
Online Access:https://insu.hal.science/insu-02909117
https://insu.hal.science/insu-02909117/document
https://insu.hal.science/insu-02909117/file/2020GL088785.pdf
https://doi.org/10.1029/2020GL088785
id ftinspolytechpar:oai:HAL:insu-02909117v1
record_format openpolar
institution Open Polar
collection HAL de l'Institut Polytechnique de Paris
op_collection_id ftinspolytechpar
language English
topic [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 [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
Listowski, Constantino
Rojo, Mathias
Claud, Chantal
Delanoë, Julien
Rysman, Jean-François
Cazenave, Quitterie
Noer, G.
New Insights into the Vertical Structure of Clouds in Polar Lows, using Radar‐Lidar Satellite Observations
topic_facet [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 International audience For the first time, we characterize the vertical distribution of cloud microphysical properties in polar lows (PLs). We base our investigation on colocations found between A-Train satellites overpasses and 82 PL occurrences evidenced from AVHRR observations in the Nordic Seas. We use the raDAR/liDAR DARDAR satellite cloud products to retrieve the thermodynamic phase and ice microphysical properties of clouds (ice water content [IWC] and ice crystal effective radius [r eff ]). Two thirds of the investigated PLs show cloud tops higher than commonly documented (5 km), and up to 9 km. PLs are largely dominated by the ice phase, with more supercooled liquid occurrences in the eye. We also show that spiraliform clouds have larger average IWC in the few kilometers below cloud top, by up to a factor of 2, compared to comma-shaped PLs. Plain Language Summary Polar lows are intense maritime cyclones posing serious threats to mariners and coastal populations. Due to their limited size and sudden development, operational forecast struggles to correctly predict them. Additionally, the limited amount of observational constraints renders improvements of simulations difficult. We provide the first statistical analyses of cloud microphysical properties of these storms using radar and lidar satellite observations. We demonstrate much higher cloud tops than usually assumed. We highlight the cloud phase, describe the vertical distribution of ice mass and crystal size, and stress some differences between spiraliform and comma-shaped cyclones. These new constraints can be readily used to improve polar lows' simulations.
author2 Laboratoire Atmosphères, Milieux, Observations Spatiales (LATMOS)
Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)
DAM Île-de-France (DAM/DIF)
Direction des Applications Militaires (DAM)
Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)
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-PSL)
Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-École normale supérieure - Paris (ENS-PSL)
Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)
SPACE - LATMOS
Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)
Norwegian Meteorological Institute Oslo (MET)
format Article in Journal/Newspaper
author Listowski, Constantino
Rojo, Mathias
Claud, Chantal
Delanoë, Julien
Rysman, Jean-François
Cazenave, Quitterie
Noer, G.
author_facet Listowski, Constantino
Rojo, Mathias
Claud, Chantal
Delanoë, Julien
Rysman, Jean-François
Cazenave, Quitterie
Noer, G.
author_sort Listowski, Constantino
title New Insights into the Vertical Structure of Clouds in Polar Lows, using Radar‐Lidar Satellite Observations
title_short New Insights into the Vertical Structure of Clouds in Polar Lows, using Radar‐Lidar Satellite Observations
title_full New Insights into the Vertical Structure of Clouds in Polar Lows, using Radar‐Lidar Satellite Observations
title_fullStr New Insights into the Vertical Structure of Clouds in Polar Lows, using Radar‐Lidar Satellite Observations
title_full_unstemmed New Insights into the Vertical Structure of Clouds in Polar Lows, using Radar‐Lidar Satellite Observations
title_sort new insights into the vertical structure of clouds in polar lows, using radar‐lidar satellite observations
publisher HAL CCSD
publishDate 2020
url https://insu.hal.science/insu-02909117
https://insu.hal.science/insu-02909117/document
https://insu.hal.science/insu-02909117/file/2020GL088785.pdf
https://doi.org/10.1029/2020GL088785
genre Nordic Seas
genre_facet Nordic Seas
op_source ISSN: 0094-8276
EISSN: 1944-8007
Geophysical Research Letters
https://insu.hal.science/insu-02909117
Geophysical Research Letters, 2020, 47 (17), pp.e2020GL088785. ⟨10.1029/2020GL088785⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1029/2020GL088785
insu-02909117
https://insu.hal.science/insu-02909117
https://insu.hal.science/insu-02909117/document
https://insu.hal.science/insu-02909117/file/2020GL088785.pdf
doi:10.1029/2020GL088785
op_rights info:eu-repo/semantics/OpenAccess
op_doi https://doi.org/10.1029/2020GL088785
container_title Geophysical Research Letters
container_volume 47
container_issue 17
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spelling ftinspolytechpar:oai:HAL:insu-02909117v1 2024-06-16T07:41:36+00:00 New Insights into the Vertical Structure of Clouds in Polar Lows, using Radar‐Lidar Satellite Observations Listowski, Constantino Rojo, Mathias Claud, Chantal Delanoë, Julien Rysman, Jean-François Cazenave, Quitterie Noer, G. Laboratoire Atmosphères, Milieux, Observations Spatiales (LATMOS) Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS) DAM Île-de-France (DAM/DIF) Direction des Applications Militaires (DAM) Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA) 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-PSL) Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-École normale supérieure - Paris (ENS-PSL) Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL) SPACE - LATMOS Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS) Norwegian Meteorological Institute Oslo (MET) 2020 https://insu.hal.science/insu-02909117 https://insu.hal.science/insu-02909117/document https://insu.hal.science/insu-02909117/file/2020GL088785.pdf https://doi.org/10.1029/2020GL088785 en eng HAL CCSD American Geophysical Union info:eu-repo/semantics/altIdentifier/doi/10.1029/2020GL088785 insu-02909117 https://insu.hal.science/insu-02909117 https://insu.hal.science/insu-02909117/document https://insu.hal.science/insu-02909117/file/2020GL088785.pdf doi:10.1029/2020GL088785 info:eu-repo/semantics/OpenAccess ISSN: 0094-8276 EISSN: 1944-8007 Geophysical Research Letters https://insu.hal.science/insu-02909117 Geophysical Research Letters, 2020, 47 (17), pp.e2020GL088785. ⟨10.1029/2020GL088785⟩ [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 2020 ftinspolytechpar https://doi.org/10.1029/2020GL088785 2024-05-19T23:44:35Z International audience For the first time, we characterize the vertical distribution of cloud microphysical properties in polar lows (PLs). We base our investigation on colocations found between A-Train satellites overpasses and 82 PL occurrences evidenced from AVHRR observations in the Nordic Seas. We use the raDAR/liDAR DARDAR satellite cloud products to retrieve the thermodynamic phase and ice microphysical properties of clouds (ice water content [IWC] and ice crystal effective radius [r eff ]). Two thirds of the investigated PLs show cloud tops higher than commonly documented (5 km), and up to 9 km. PLs are largely dominated by the ice phase, with more supercooled liquid occurrences in the eye. We also show that spiraliform clouds have larger average IWC in the few kilometers below cloud top, by up to a factor of 2, compared to comma-shaped PLs. Plain Language Summary Polar lows are intense maritime cyclones posing serious threats to mariners and coastal populations. Due to their limited size and sudden development, operational forecast struggles to correctly predict them. Additionally, the limited amount of observational constraints renders improvements of simulations difficult. We provide the first statistical analyses of cloud microphysical properties of these storms using radar and lidar satellite observations. We demonstrate much higher cloud tops than usually assumed. We highlight the cloud phase, describe the vertical distribution of ice mass and crystal size, and stress some differences between spiraliform and comma-shaped cyclones. These new constraints can be readily used to improve polar lows' simulations. Article in Journal/Newspaper Nordic Seas HAL de l'Institut Polytechnique de Paris Geophysical Research Letters 47 17