ExoMars TGO/NOMAD-UVIS Vertical Profiles of Ozone: 2. The High-Altitude Layers of Atmospheric Ozone

This is an open access article under the terms of the Creative Commons Attribution-NonCommercial-NoDerivs License, which permits use and distribution in any medium, provided the original work is properly cited, the use is non-commercial and no modifications or adaptations are made.

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Autores: Khayat, Alain S. J., Smith, Michael D., Wolff, Michael, Daerden, Frank, Neary, Lori, Patel, Manish R., Piccialli, Arianna, Vandaele, Ann Carine, Thomas, Ian R., Ristic, Bojan, Mason, Jon, Willame, Yannick, Depiesse, Cedric, Bellucci, Giancarlo, López-Moreno, José Juan
Tipo de recurso: artículo
Estado:Versión publicada
Fecha de publicación:2021
País:España
Institución:Consejo Superior de Investigaciones Científicas (CSIC)
Repositorio:DIGITAL.CSIC. Repositorio Institucional del CSIC
OAI Identifier:oai:digital.csic.es:10261/264152
Acceso en línea:http://hdl.handle.net/10261/264152
Access Level:acceso abierto
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dc.title.none.fl_str_mv ExoMars TGO/NOMAD-UVIS Vertical Profiles of Ozone: 2. The High-Altitude Layers of Atmospheric Ozone
title ExoMars TGO/NOMAD-UVIS Vertical Profiles of Ozone: 2. The High-Altitude Layers of Atmospheric Ozone
spellingShingle ExoMars TGO/NOMAD-UVIS Vertical Profiles of Ozone: 2. The High-Altitude Layers of Atmospheric Ozone
Khayat, Alain S. J.
title_short ExoMars TGO/NOMAD-UVIS Vertical Profiles of Ozone: 2. The High-Altitude Layers of Atmospheric Ozone
title_full ExoMars TGO/NOMAD-UVIS Vertical Profiles of Ozone: 2. The High-Altitude Layers of Atmospheric Ozone
title_fullStr ExoMars TGO/NOMAD-UVIS Vertical Profiles of Ozone: 2. The High-Altitude Layers of Atmospheric Ozone
title_full_unstemmed ExoMars TGO/NOMAD-UVIS Vertical Profiles of Ozone: 2. The High-Altitude Layers of Atmospheric Ozone
title_sort ExoMars TGO/NOMAD-UVIS Vertical Profiles of Ozone: 2. The High-Altitude Layers of Atmospheric Ozone
dc.creator.none.fl_str_mv Khayat, Alain S. J.
Smith, Michael D.
Wolff, Michael
Daerden, Frank
Neary, Lori
Patel, Manish R.
Piccialli, Arianna
Vandaele, Ann Carine
Thomas, Ian R.
Ristic, Bojan
Mason, Jon
Willame, Yannick
Depiesse, Cedric
Bellucci, Giancarlo
López-Moreno, José Juan
author Khayat, Alain S. J.
author_facet Khayat, Alain S. J.
Smith, Michael D.
Wolff, Michael
Daerden, Frank
Neary, Lori
Patel, Manish R.
Piccialli, Arianna
Vandaele, Ann Carine
Thomas, Ian R.
Ristic, Bojan
Mason, Jon
Willame, Yannick
Depiesse, Cedric
Bellucci, Giancarlo
López-Moreno, José Juan
author_role author
author2 Smith, Michael D.
Wolff, Michael
Daerden, Frank
Neary, Lori
Patel, Manish R.
Piccialli, Arianna
Vandaele, Ann Carine
Thomas, Ian R.
Ristic, Bojan
Mason, Jon
Willame, Yannick
Depiesse, Cedric
Bellucci, Giancarlo
López-Moreno, José Juan
author2_role author
author
author
author
author
author
author
author
author
author
author
author
author
author
dc.contributor.none.fl_str_mv NASA
Belgian Science Policy Office
European Commission
Ministerio de Economía y Competitividad (España)
Ministerio de Ciencia, Innovación y Universidades (España)
UK Space Agency
National Fund for Scientific Research (Belgium)
Agenzia Spaziale Italiana
Consejo Superior de Investigaciones Científicas [https://ror.org/02gfc7t72]
description This is an open access article under the terms of the Creative Commons Attribution-NonCommercial-NoDerivs License, which permits use and distribution in any medium, provided the original work is properly cited, the use is non-commercial and no modifications or adaptations are made.
publishDate 2021
dc.date.none.fl_str_mv 2021
2022
2022
dc.type.none.fl_str_mv info:eu-repo/semantics/article
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dc.identifier.none.fl_str_mv http://hdl.handle.net/10261/264152
url http://hdl.handle.net/10261/264152
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info:eu-repo/grantAgreement/AEI/Plan Estatal de Investigación Científica y Técnica y de Innovación 2013-2016/ESP2017-87143-R
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http://dx.doi.org/10.1029/2021JE006834

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dc.publisher.none.fl_str_mv American Geophysical Union
publisher.none.fl_str_mv American Geophysical Union
dc.source.none.fl_str_mv reponame:DIGITAL.CSIC. Repositorio Institucional del CSIC
instname:Consejo Superior de Investigaciones Científicas (CSIC)
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spelling ExoMars TGO/NOMAD-UVIS Vertical Profiles of Ozone: 2. The High-Altitude Layers of Atmospheric OzoneKhayat, Alain S. J.Smith, Michael D.Wolff, MichaelDaerden, FrankNeary, LoriPatel, Manish R.Piccialli, AriannaVandaele, Ann CarineThomas, Ian R.Ristic, BojanMason, JonWillame, YannickDepiesse, CedricBellucci, GiancarloLópez-Moreno, José JuanThis is an open access article under the terms of the Creative Commons Attribution-NonCommercial-NoDerivs License, which permits use and distribution in any medium, provided the original work is properly cited, the use is non-commercial and no modifications or adaptations are made.Solar occultations performed by the Nadir and Occultation for MArs Discovery (NOMAD) ultraviolet and visible spectrometer (UVIS) onboard the ExoMars Trace Gas Orbiter (TGO) have provided a comprehensive mapping of atmospheric ozone density. The observations here extend over a full Mars year (MY) between April 21, 2018 at the beginning of the TGO science operations during late northern summer on Mars (MY 34, Ls = 163°) and March 9, 2020 (MY 35). UVIS provided transmittance spectra of the Martian atmosphere allowing measurements of the vertical distribution of ozone density using its Hartley absorption band (200–300 nm). The overall comparison to water vapor is found in the companion paper to this work (Patel et al., 2021, https://doi.org/10.1029/2021JE006837). Our findings indicate the presence of (a) a high-altitude peak of ozone between 40 and 60 km in altitude over the north polar latitudes for at least 45% of the Martian year during midnorthern spring, late northern summer-early southern spring, and late southern summer, and (b) a second, but more prominent, high-altitude ozone peak in the south polar latitudes, lasting for at least 60% of the year including the southern autumn and winter seasons. When present, both high-altitude peaks are observed in the sunrise and sunset occultations, suggesting that the layers could persist during the day. Results from the Mars general circulation models predict the general behavior of these peaks of ozone and are used in an attempt to further our understanding of the chemical processes controlling high-altitude ozone on Mars. © 2021 The Authors. This article has been contributed to by US Government employees and their work is in the public domain in the USA.This work was supported by the NASA's Mars Program Office under WBS 604796, “Participation in the TGO/NOMAD Investigation of Trace Gases on Mars.” The material was based upon the work supported by the NASA under award No. 80GSFC21M0002. The NOMAD experiment was led by the Royal Belgian Institute for Space Aeronomy (IASB-BIRA), assisted by Co-PI teams from Spain (IAA-CSIC), Italy (INAF-IAPS), and the United Kingdom (Open University). This project acknowledges funding by the Belgian Science Policy Office (BELSPO), with the financial and contractual coordination by the ESA Prodex Office (PEA 4000103401, 4000121493), by the Spanish Ministry of Science and Innovation (MCIU) and by the European funds under grants PGC2018-101836-B-I00 and ESP2017-87143-R (MINECO/FEDER), as well as by the UK Space Agency through Grants ST/V002295/1, ST/P001262/1, ST/S00145X/1, and ST/V005332/1 and Italian Space Agency through Grant 2018-2-HH.0. This work was supported by the Belgian Fonds de la Recherche Scientifique—FNRS under Grant No. 30442502 (ET_HOME). This project has received funding from the European Union's Horizon 2020 research and innovation programme under Grant Agreement No. 101004052 (RoadMap project). The IAA/CSIC team acknowledges financial support from the State Agency for Research of the Spanish MCIU through the “Center of Excellence Severo Ochoa” award for the Instituto de Astrofísica de Andalucía (SEV-2017-0709). US investigators were supported by the National Aeronautics and Space Administration. Canadian investigators were supported by the Canadian Space Agency.Peer reviewedAmerican Geophysical UnionNASABelgian Science Policy OfficeEuropean CommissionMinisterio de Economía y Competitividad (España)Ministerio de Ciencia, Innovación y Universidades (España)UK Space AgencyNational Fund for Scientific Research (Belgium)Agenzia Spaziale ItalianaConsejo Superior de Investigaciones Científicas [https://ror.org/02gfc7t72]202220222021info:eu-repo/semantics/articlehttp://purl.org/coar/resource_type/c_6501Publisher's versioninfo:eu-repo/semantics/publishedVersionhttp://hdl.handle.net/10261/264152reponame:DIGITAL.CSIC. Repositorio Institucional del CSICinstname:Consejo Superior de Investigaciones Científicas (CSIC)Inglés#PLACEHOLDER_PARENT_METADATA_VALUE##PLACEHOLDER_PARENT_METADATA_VALUE##PLACEHOLDER_PARENT_METADATA_VALUE##PLACEHOLDER_PARENT_METADATA_VALUE#info:eu-repo/grantAgreement/AEI/Plan Estatal de Investigación Científica y Técnica y de Innovación 2017-2020/PGC2018-101836-B-I00info:eu-repo/grantAgreement/AEI/Plan Estatal de Investigación Científica y Técnica y de Innovación 2013-2016/ESP2017-87143-Rinfo:eu-repo/grantAgreement/EC/H2020/101004052info:eu-repo/grantAgreement/MICINN//SEV-2017-0709http://dx.doi.org/10.1029/2021JE006834Síinfo:eu-repo/semantics/openAccessoai:digital.csic.es:10261/2641522026-05-22T06:33:51Z
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