OClO slant column densities derived from GOMOS averaged transmittance measurements

The Global Ozone Monitoring by Occultation of Stars (GOMOS) instrument on board the European platform ENVISAT (ENVironment SATellite) was dedicated to the study of the of Earth's atmosphere using the stellar occultation technique. The spectral range of the GOMOS spectrometer extends from the UV...

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Published in:Atmospheric Measurement Techniques
Main Authors: Tétard, C., Fussen, D., Vanhellemont, F., Bingen, C., Dekemper, E., Mateshvili, N., Pieroux, D., Robert, Cédric, Kyrölä, E., Tamminen, J., Sofieva, Viktoria, Hauchecorne, Alain, Dalaudier, Francis, Bertaux, Jean-Loup, Fanton D'Andon, O., Barrot, G., Blanot, L., Dehn, A., Saavedra De Miguel, L.
Other Authors: Belgian Institute for Space Aeronomy / Institut d'Aéronomie Spatiale de Belgique (BIRA-IASB), Finnish Meteorological Institute (FMI), 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), Analytic and Computational Research, Inc. - Earth Sciences (ACRI-ST), European Space Research Institute (ESRIN), European Space Agency (ESA)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2013
Subjects:
Online Access:https://hal.archives-ouvertes.fr/hal-00879784
https://hal.archives-ouvertes.fr/hal-00879784/document
https://hal.archives-ouvertes.fr/hal-00879784/file/amt-6-2953-2013.pdf
https://doi.org/10.5194/amt-6-2953-2013
id ftccsdartic:oai:HAL:hal-00879784v1
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 [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]
Tétard, C.
Fussen, D.
Vanhellemont, F.
Bingen, C.
Dekemper, E.
Mateshvili, N.
Pieroux, D.
Robert, Cédric,
Kyrölä, E.
Tamminen, J.
Sofieva, Viktoria
Hauchecorne, Alain
Dalaudier, Francis
Bertaux, Jean-Loup
Fanton D'Andon, O.
Barrot, G.
Blanot, L.
Dehn, A.
Saavedra De Miguel, L.
OClO slant column densities derived from GOMOS averaged transmittance measurements
topic_facet [PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph]
description The Global Ozone Monitoring by Occultation of Stars (GOMOS) instrument on board the European platform ENVISAT (ENVironment SATellite) was dedicated to the study of the of Earth's atmosphere using the stellar occultation technique. The spectral range of the GOMOS spectrometer extends from the UV (ultra violet) to the near infrared, allowing for the retrieval of species such as O3, NO2, NO3, H2O, O2, air density, aerosol extinction and OClO. Nevertheless, OClO cannot be retrieved using a single GOMOS measurement because of the weak signal-to-noise ratio and the small optical thickness associated with this molecule. We present here the method used to detect this molecule by using several GOMOS measurements. It is based on a two-step approach. First, several co-located measurements are combined in a statistical way to build an averaged measurement with a higher signal-to-noise ratio; then, a differential optical absorption spectroscopy (DOAS) method is applied to retrieve OClO slant column densities (SCD). The statistics of the sets of GOMOS measurements used to build the averaged measurement and the spectral window selection are analyzed. The obtained retrievals are compared to results from two balloon-borne instruments. It appears that the inter-comparisons of OClO are generally satisfying (relative differences are about 15-60%). Two nighttime climatologies of OClO based on GOMOS averaged measurements are presented. The first depicts annual global pictures of OClO from 2003 to 2011. From this climatology, the presence of an OClO SCD peak in the equatorial region at about 35 km is confirmed and strong OClO SCD in both polar regions are observed (more than 1016 cm−2 in the Antarctic region and slightly less in the Arctic region), a sign of chlorine activation. The second climatology is a monthly time series. It clearly shows the chlorine activation of the lower stratosphere during winter. Moreover the equatorial OClO SCD peak is observed during all years without any significant variations. This very promising ...
author2 Belgian Institute for Space Aeronomy / Institut d'Aéronomie Spatiale de Belgique (BIRA-IASB)
Finnish Meteorological Institute (FMI)
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)
Analytic and Computational Research, Inc. - Earth Sciences (ACRI-ST)
European Space Research Institute (ESRIN)
European Space Agency (ESA)
format Article in Journal/Newspaper
author Tétard, C.
Fussen, D.
Vanhellemont, F.
Bingen, C.
Dekemper, E.
Mateshvili, N.
Pieroux, D.
Robert, Cédric,
Kyrölä, E.
Tamminen, J.
Sofieva, Viktoria
Hauchecorne, Alain
Dalaudier, Francis
Bertaux, Jean-Loup
Fanton D'Andon, O.
Barrot, G.
Blanot, L.
Dehn, A.
Saavedra De Miguel, L.
author_facet Tétard, C.
Fussen, D.
Vanhellemont, F.
Bingen, C.
Dekemper, E.
Mateshvili, N.
Pieroux, D.
Robert, Cédric,
Kyrölä, E.
Tamminen, J.
Sofieva, Viktoria
Hauchecorne, Alain
Dalaudier, Francis
Bertaux, Jean-Loup
Fanton D'Andon, O.
Barrot, G.
Blanot, L.
Dehn, A.
Saavedra De Miguel, L.
author_sort Tétard, C.
title OClO slant column densities derived from GOMOS averaged transmittance measurements
title_short OClO slant column densities derived from GOMOS averaged transmittance measurements
title_full OClO slant column densities derived from GOMOS averaged transmittance measurements
title_fullStr OClO slant column densities derived from GOMOS averaged transmittance measurements
title_full_unstemmed OClO slant column densities derived from GOMOS averaged transmittance measurements
title_sort oclo slant column densities derived from gomos averaged transmittance measurements
publisher HAL CCSD
publishDate 2013
url https://hal.archives-ouvertes.fr/hal-00879784
https://hal.archives-ouvertes.fr/hal-00879784/document
https://hal.archives-ouvertes.fr/hal-00879784/file/amt-6-2953-2013.pdf
https://doi.org/10.5194/amt-6-2953-2013
geographic Arctic
Antarctic
The Antarctic
geographic_facet Arctic
Antarctic
The Antarctic
genre Antarc*
Antarctic
Arctic
genre_facet Antarc*
Antarctic
Arctic
op_source ISSN: 1867-1381
EISSN: 1867-8548
Atmospheric Measurement Techniques
https://hal.archives-ouvertes.fr/hal-00879784
Atmospheric Measurement Techniques, European Geosciences Union, 2013, 6 (11), pp.2953-2964. ⟨10.5194/amt-6-2953-2013⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.5194/amt-6-2953-2013
hal-00879784
https://hal.archives-ouvertes.fr/hal-00879784
https://hal.archives-ouvertes.fr/hal-00879784/document
https://hal.archives-ouvertes.fr/hal-00879784/file/amt-6-2953-2013.pdf
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op_doi https://doi.org/10.5194/amt-6-2953-2013
container_title Atmospheric Measurement Techniques
container_volume 6
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spelling ftccsdartic:oai:HAL:hal-00879784v1 2023-05-15T13:47:05+02:00 OClO slant column densities derived from GOMOS averaged transmittance measurements Tétard, C. Fussen, D. Vanhellemont, F. Bingen, C. Dekemper, E. Mateshvili, N. Pieroux, D. Robert, Cédric, Kyrölä, E. Tamminen, J. Sofieva, Viktoria Hauchecorne, Alain Dalaudier, Francis Bertaux, Jean-Loup Fanton D'Andon, O. Barrot, G. Blanot, L. Dehn, A. Saavedra De Miguel, L. Belgian Institute for Space Aeronomy / Institut d'Aéronomie Spatiale de Belgique (BIRA-IASB) Finnish Meteorological Institute (FMI) 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) Analytic and Computational Research, Inc. - Earth Sciences (ACRI-ST) European Space Research Institute (ESRIN) European Space Agency (ESA) 2013 https://hal.archives-ouvertes.fr/hal-00879784 https://hal.archives-ouvertes.fr/hal-00879784/document https://hal.archives-ouvertes.fr/hal-00879784/file/amt-6-2953-2013.pdf https://doi.org/10.5194/amt-6-2953-2013 en eng HAL CCSD European Geosciences Union info:eu-repo/semantics/altIdentifier/doi/10.5194/amt-6-2953-2013 hal-00879784 https://hal.archives-ouvertes.fr/hal-00879784 https://hal.archives-ouvertes.fr/hal-00879784/document https://hal.archives-ouvertes.fr/hal-00879784/file/amt-6-2953-2013.pdf doi:10.5194/amt-6-2953-2013 info:eu-repo/semantics/OpenAccess ISSN: 1867-1381 EISSN: 1867-8548 Atmospheric Measurement Techniques https://hal.archives-ouvertes.fr/hal-00879784 Atmospheric Measurement Techniques, European Geosciences Union, 2013, 6 (11), pp.2953-2964. ⟨10.5194/amt-6-2953-2013⟩ [PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph] info:eu-repo/semantics/article Journal articles 2013 ftccsdartic https://doi.org/10.5194/amt-6-2953-2013 2021-11-21T03:02:55Z The Global Ozone Monitoring by Occultation of Stars (GOMOS) instrument on board the European platform ENVISAT (ENVironment SATellite) was dedicated to the study of the of Earth's atmosphere using the stellar occultation technique. The spectral range of the GOMOS spectrometer extends from the UV (ultra violet) to the near infrared, allowing for the retrieval of species such as O3, NO2, NO3, H2O, O2, air density, aerosol extinction and OClO. Nevertheless, OClO cannot be retrieved using a single GOMOS measurement because of the weak signal-to-noise ratio and the small optical thickness associated with this molecule. We present here the method used to detect this molecule by using several GOMOS measurements. It is based on a two-step approach. First, several co-located measurements are combined in a statistical way to build an averaged measurement with a higher signal-to-noise ratio; then, a differential optical absorption spectroscopy (DOAS) method is applied to retrieve OClO slant column densities (SCD). The statistics of the sets of GOMOS measurements used to build the averaged measurement and the spectral window selection are analyzed. The obtained retrievals are compared to results from two balloon-borne instruments. It appears that the inter-comparisons of OClO are generally satisfying (relative differences are about 15-60%). Two nighttime climatologies of OClO based on GOMOS averaged measurements are presented. The first depicts annual global pictures of OClO from 2003 to 2011. From this climatology, the presence of an OClO SCD peak in the equatorial region at about 35 km is confirmed and strong OClO SCD in both polar regions are observed (more than 1016 cm−2 in the Antarctic region and slightly less in the Arctic region), a sign of chlorine activation. The second climatology is a monthly time series. It clearly shows the chlorine activation of the lower stratosphere during winter. Moreover the equatorial OClO SCD peak is observed during all years without any significant variations. This very promising ... Article in Journal/Newspaper Antarc* Antarctic Arctic Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) Arctic Antarctic The Antarctic Atmospheric Measurement Techniques 6 11 2953 2964