Exploring the signature of polar lows in infrasound: the 19–20 November 2008 cases

International audience We report in this study the infrasound signal measured consistently at four stations in Fennoscandia, associated with the development of two intense cyclones, called polar lows, over the Norwegian Sea. When conditions of propagation are favourable, the infrasound signal comes...

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Published in:Tellus A: Dynamic Meteorology and Oceanography
Main Authors: Claud, Chantal, Dalaudier, Francis, Kero, Johan, Le Pichon, Alexis, Hauchecorne, Alain, Rojo, Maxence, Blanc, Elisabeth, Liszka, Ludwik
Other Authors: 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), STRATO - LATMOS, Laboratoire Atmosphères, Milieux, Observations Spatiales (LATMOS), Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS), Swedish Institute of Space Physics Kiruna (IRF), 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)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2017
Subjects:
Online Access:https://hal-insu.archives-ouvertes.fr/insu-01729993
https://hal-insu.archives-ouvertes.fr/insu-01729993/document
https://hal-insu.archives-ouvertes.fr/insu-01729993/file/Exploring%20the%20signature%20of%20polar%20lows%20in%20infrasound%20the%2019%2020%20November%202008%20cases.pdf
https://doi.org/10.1080/16000870.2017.1338885
id ftccsdartic:oai:HAL:insu-01729993v1
record_format openpolar
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 polar lows
infrasound
convection
[PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph]
spellingShingle polar lows
infrasound
convection
[PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph]
Claud, Chantal
Dalaudier, Francis
Kero, Johan
Le Pichon, Alexis
Hauchecorne, Alain
Rojo, Maxence
Blanc, Elisabeth
Liszka, Ludwik
Exploring the signature of polar lows in infrasound: the 19–20 November 2008 cases
topic_facet polar lows
infrasound
convection
[PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph]
description International audience We report in this study the infrasound signal measured consistently at four stations in Fennoscandia, associated with the development of two intense cyclones, called polar lows, over the Norwegian Sea. When conditions of propagation are favourable, the infrasound signal comes from the direction of the polar lows, and it follows their track. The results thus, tend to confirm those of a previous study who claimed that an outbreak of three polar lows generated clear infrasound to distances up to 1000 km, according to measurements acquired in Northern Norway and on Svalbard. Because the conditions of propagation of infrasound depend on the state of the atmosphere between the sources and the receivers, signals may remain undetected, which limits the capability of a systematic early warning system, and also of a global monitoring of polar lows. However, the recorded signals might reflect on-going source processes, since convection associated with the polar lows is detected using microwave satellite observations in the areas from which the signals emanate. This suggests that at least part of the signal is due to turbulence induced by convection, in agreement with the earlier study. Nevertheless, more evidence of broadband infrasound measurements of polar low cases have to be examined in order to be able to fully assess the role of other possible sources (swell, surf, lightnings, …). The addition in Northern Norway in late 2013 of the IS37 infrasound station of the International Monitoring Network, developed for the verification of the Comprehensive nuclear-Test-ban Treaty, will provide new opportunities to further investigate this issue.
author2 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)
STRATO - LATMOS
Laboratoire Atmosphères, Milieux, Observations Spatiales (LATMOS)
Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)
Swedish Institute of Space Physics Kiruna (IRF)
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)
format Article in Journal/Newspaper
author Claud, Chantal
Dalaudier, Francis
Kero, Johan
Le Pichon, Alexis
Hauchecorne, Alain
Rojo, Maxence
Blanc, Elisabeth
Liszka, Ludwik
author_facet Claud, Chantal
Dalaudier, Francis
Kero, Johan
Le Pichon, Alexis
Hauchecorne, Alain
Rojo, Maxence
Blanc, Elisabeth
Liszka, Ludwik
author_sort Claud, Chantal
title Exploring the signature of polar lows in infrasound: the 19–20 November 2008 cases
title_short Exploring the signature of polar lows in infrasound: the 19–20 November 2008 cases
title_full Exploring the signature of polar lows in infrasound: the 19–20 November 2008 cases
title_fullStr Exploring the signature of polar lows in infrasound: the 19–20 November 2008 cases
title_full_unstemmed Exploring the signature of polar lows in infrasound: the 19–20 November 2008 cases
title_sort exploring the signature of polar lows in infrasound: the 19–20 november 2008 cases
publisher HAL CCSD
publishDate 2017
url https://hal-insu.archives-ouvertes.fr/insu-01729993
https://hal-insu.archives-ouvertes.fr/insu-01729993/document
https://hal-insu.archives-ouvertes.fr/insu-01729993/file/Exploring%20the%20signature%20of%20polar%20lows%20in%20infrasound%20the%2019%2020%20November%202008%20cases.pdf
https://doi.org/10.1080/16000870.2017.1338885
geographic Svalbard
Norwegian Sea
Norway
geographic_facet Svalbard
Norwegian Sea
Norway
genre Fennoscandia
Northern Norway
Norwegian Sea
Svalbard
genre_facet Fennoscandia
Northern Norway
Norwegian Sea
Svalbard
op_source ISSN: 0280-6495
EISSN: 1600-0870
Tellus A
https://hal-insu.archives-ouvertes.fr/insu-01729993
Tellus A, Co-Action Publishing, 2017, 69 (1), ⟨10.1080/16000870.2017.1338885⟩
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https://hal-insu.archives-ouvertes.fr/insu-01729993
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doi:10.1080/16000870.2017.1338885
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container_title Tellus A: Dynamic Meteorology and Oceanography
container_volume 69
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spelling ftccsdartic:oai:HAL:insu-01729993v1 2023-05-15T16:12:10+02:00 Exploring the signature of polar lows in infrasound: the 19–20 November 2008 cases Claud, Chantal Dalaudier, Francis Kero, Johan Le Pichon, Alexis Hauchecorne, Alain Rojo, Maxence Blanc, Elisabeth Liszka, Ludwik 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) STRATO - LATMOS Laboratoire Atmosphères, Milieux, Observations Spatiales (LATMOS) Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS) Swedish Institute of Space Physics Kiruna (IRF) 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) 2017-11-29 https://hal-insu.archives-ouvertes.fr/insu-01729993 https://hal-insu.archives-ouvertes.fr/insu-01729993/document https://hal-insu.archives-ouvertes.fr/insu-01729993/file/Exploring%20the%20signature%20of%20polar%20lows%20in%20infrasound%20the%2019%2020%20November%202008%20cases.pdf https://doi.org/10.1080/16000870.2017.1338885 en eng HAL CCSD Co-Action Publishing info:eu-repo/semantics/altIdentifier/doi/10.1080/16000870.2017.1338885 insu-01729993 https://hal-insu.archives-ouvertes.fr/insu-01729993 https://hal-insu.archives-ouvertes.fr/insu-01729993/document https://hal-insu.archives-ouvertes.fr/insu-01729993/file/Exploring%20the%20signature%20of%20polar%20lows%20in%20infrasound%20the%2019%2020%20November%202008%20cases.pdf doi:10.1080/16000870.2017.1338885 http://creativecommons.org/licenses/by-nc/ info:eu-repo/semantics/OpenAccess CC-BY-NC ISSN: 0280-6495 EISSN: 1600-0870 Tellus A https://hal-insu.archives-ouvertes.fr/insu-01729993 Tellus A, Co-Action Publishing, 2017, 69 (1), ⟨10.1080/16000870.2017.1338885⟩ polar lows infrasound convection [PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph] info:eu-repo/semantics/article Journal articles 2017 ftccsdartic https://doi.org/10.1080/16000870.2017.1338885 2021-11-21T00:37:03Z International audience We report in this study the infrasound signal measured consistently at four stations in Fennoscandia, associated with the development of two intense cyclones, called polar lows, over the Norwegian Sea. When conditions of propagation are favourable, the infrasound signal comes from the direction of the polar lows, and it follows their track. The results thus, tend to confirm those of a previous study who claimed that an outbreak of three polar lows generated clear infrasound to distances up to 1000 km, according to measurements acquired in Northern Norway and on Svalbard. Because the conditions of propagation of infrasound depend on the state of the atmosphere between the sources and the receivers, signals may remain undetected, which limits the capability of a systematic early warning system, and also of a global monitoring of polar lows. However, the recorded signals might reflect on-going source processes, since convection associated with the polar lows is detected using microwave satellite observations in the areas from which the signals emanate. This suggests that at least part of the signal is due to turbulence induced by convection, in agreement with the earlier study. Nevertheless, more evidence of broadband infrasound measurements of polar low cases have to be examined in order to be able to fully assess the role of other possible sources (swell, surf, lightnings, …). The addition in Northern Norway in late 2013 of the IS37 infrasound station of the International Monitoring Network, developed for the verification of the Comprehensive nuclear-Test-ban Treaty, will provide new opportunities to further investigate this issue. Article in Journal/Newspaper Fennoscandia Northern Norway Norwegian Sea Svalbard Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) Svalbard Norwegian Sea Norway Tellus A: Dynamic Meteorology and Oceanography 69 1 1338885