Origin of the January–April 2004 increase in stratospheric NO2 observed in the northern polar latitudes

International audience Large increase in stratospheric NO2 content has been observed during the 2003–2004 Arctic winter. The first one, in early November 2003 is well documented and is due to a strong solar protons event. A second event occurred on January 22, 2004, leading to a large amount of NO2...

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Published in:Geophysical Research Letters
Main Authors: Renard, Jean-Baptiste, Blelly, Pierre-Louis, Bourgeois, Quentin, Chartier, Michel, Goutail, Florence, Orsolini, Y.J.
Other Authors: Laboratoire de physique et chimie de l'environnement (LPCE), Institut national des sciences de l'Univers (INSU - CNRS)-Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS), Service d'aéronomie (SA), 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), Norwegian Institute for Air Research (NILU)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2006
Subjects:
Online Access:https://hal.science/hal-00083635
https://hal.science/hal-00083635/document
https://hal.science/hal-00083635/file/Renard_et_al-2006-Geophysical_Research_Letters.pdf
https://doi.org/10.1029/2005GL025450
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spelling ftunivorleans:oai:HAL:hal-00083635v1 2023-11-12T04:13:03+01:00 Origin of the January–April 2004 increase in stratospheric NO2 observed in the northern polar latitudes Renard, Jean-Baptiste Blelly, Pierre-Louis Bourgeois, Quentin Chartier, Michel Goutail, Florence Orsolini, Y.J. Laboratoire de physique et chimie de l'environnement (LPCE) Institut national des sciences de l'Univers (INSU - CNRS)-Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS) Service d'aéronomie (SA) 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) Norwegian Institute for Air Research (NILU) 2006 https://hal.science/hal-00083635 https://hal.science/hal-00083635/document https://hal.science/hal-00083635/file/Renard_et_al-2006-Geophysical_Research_Letters.pdf https://doi.org/10.1029/2005GL025450 en eng HAL CCSD American Geophysical Union info:eu-repo/semantics/altIdentifier/doi/10.1029/2005GL025450 hal-00083635 https://hal.science/hal-00083635 https://hal.science/hal-00083635/document https://hal.science/hal-00083635/file/Renard_et_al-2006-Geophysical_Research_Letters.pdf doi:10.1029/2005GL025450 info:eu-repo/semantics/OpenAccess ISSN: 0094-8276 EISSN: 1944-8007 Geophysical Research Letters https://hal.science/hal-00083635 Geophysical Research Letters, 2006, 33, pp.L11801. ⟨10.1029/2005GL025450⟩ [PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph] info:eu-repo/semantics/article Journal articles 2006 ftunivorleans https://doi.org/10.1029/2005GL025450 2023-10-24T21:36:31Z International audience Large increase in stratospheric NO2 content has been observed during the 2003–2004 Arctic winter. The first one, in early November 2003 is well documented and is due to a strong solar protons event. A second event occurred on January 22, 2004, leading to a large amount of NO2 in the lower mesosphere. This second event can be analyzed using data from nighttime satellite measurements performed by the GOMOS and MIPAS instruments onboard Envisat, and by ground based column measurements performed by SAOZ. It seems that in-situ production of NO2 is located at an altitude of around 60 km associated with the precipitation of electrons with energy of a few hundred keV. These electrons originated from the high latitudes magnetosphere, and are associated with a solar coronal mass ejection. Therefore, a particular nighttime chemistry in the lower mesosphere is proposed to explain the measurements. Article in Journal/Newspaper Arctic Université d'Orléans: HAL Arctic Geophysical Research Letters 33 11
institution Open Polar
collection Université d'Orléans: HAL
op_collection_id ftunivorleans
language English
topic [PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph]
spellingShingle [PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph]
Renard, Jean-Baptiste
Blelly, Pierre-Louis
Bourgeois, Quentin
Chartier, Michel
Goutail, Florence
Orsolini, Y.J.
Origin of the January–April 2004 increase in stratospheric NO2 observed in the northern polar latitudes
topic_facet [PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph]
description International audience Large increase in stratospheric NO2 content has been observed during the 2003–2004 Arctic winter. The first one, in early November 2003 is well documented and is due to a strong solar protons event. A second event occurred on January 22, 2004, leading to a large amount of NO2 in the lower mesosphere. This second event can be analyzed using data from nighttime satellite measurements performed by the GOMOS and MIPAS instruments onboard Envisat, and by ground based column measurements performed by SAOZ. It seems that in-situ production of NO2 is located at an altitude of around 60 km associated with the precipitation of electrons with energy of a few hundred keV. These electrons originated from the high latitudes magnetosphere, and are associated with a solar coronal mass ejection. Therefore, a particular nighttime chemistry in the lower mesosphere is proposed to explain the measurements.
author2 Laboratoire de physique et chimie de l'environnement (LPCE)
Institut national des sciences de l'Univers (INSU - CNRS)-Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS)
Service d'aéronomie (SA)
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)
Norwegian Institute for Air Research (NILU)
format Article in Journal/Newspaper
author Renard, Jean-Baptiste
Blelly, Pierre-Louis
Bourgeois, Quentin
Chartier, Michel
Goutail, Florence
Orsolini, Y.J.
author_facet Renard, Jean-Baptiste
Blelly, Pierre-Louis
Bourgeois, Quentin
Chartier, Michel
Goutail, Florence
Orsolini, Y.J.
author_sort Renard, Jean-Baptiste
title Origin of the January–April 2004 increase in stratospheric NO2 observed in the northern polar latitudes
title_short Origin of the January–April 2004 increase in stratospheric NO2 observed in the northern polar latitudes
title_full Origin of the January–April 2004 increase in stratospheric NO2 observed in the northern polar latitudes
title_fullStr Origin of the January–April 2004 increase in stratospheric NO2 observed in the northern polar latitudes
title_full_unstemmed Origin of the January–April 2004 increase in stratospheric NO2 observed in the northern polar latitudes
title_sort origin of the january–april 2004 increase in stratospheric no2 observed in the northern polar latitudes
publisher HAL CCSD
publishDate 2006
url https://hal.science/hal-00083635
https://hal.science/hal-00083635/document
https://hal.science/hal-00083635/file/Renard_et_al-2006-Geophysical_Research_Letters.pdf
https://doi.org/10.1029/2005GL025450
geographic Arctic
geographic_facet Arctic
genre Arctic
genre_facet Arctic
op_source ISSN: 0094-8276
EISSN: 1944-8007
Geophysical Research Letters
https://hal.science/hal-00083635
Geophysical Research Letters, 2006, 33, pp.L11801. ⟨10.1029/2005GL025450⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1029/2005GL025450
hal-00083635
https://hal.science/hal-00083635
https://hal.science/hal-00083635/document
https://hal.science/hal-00083635/file/Renard_et_al-2006-Geophysical_Research_Letters.pdf
doi:10.1029/2005GL025450
op_rights info:eu-repo/semantics/OpenAccess
op_doi https://doi.org/10.1029/2005GL025450
container_title Geophysical Research Letters
container_volume 33
container_issue 11
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