Representativeness of single lidar stations for zonally averaged ozone profiles, their trends and attribution to proxies

International audience This paper is focusing on the representativenessof single lidar stations for zonally averaged ozone profilevariations over the middle and upper stratosphere. From thelower to the upper stratosphere, ozone profiles from singleor grouped lidar stations correlate well with zonal...

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Published in:Atmospheric Chemistry and Physics
Main Authors: Zerefos, Christos, Kapsomenakis, John, Eleftheratos, Kostas, Tourpali, Kleareti, Petropavlovskikh, Irina, Hubert, Daan, Godin-Beekmann, Sophie, Steinbrecht, Wolfgang, Frith, Stacey, Sofieva, Viktoria, Hassler, Birgit
Other Authors: Research Centre for Atmospheric Physics and Climatology Athens, Academy of Athens, Navarino Environmental Observatory (NEO), Faculty of Geology and Geoenvironment Athens, National and Kapodistrian University of Athens (NKUA), Laboratory of Atmospheric Physics Thessaloniki, Aristotle University of Thessaloniki, Cooperative Institute for Research in Environmental Sciences (CIRES), University of Colorado Boulder -National Oceanic and Atmospheric Administration (NOAA), Belgian Institute for Space Aeronomy / Institut d'Aéronomie Spatiale de Belgique (BIRA-IASB), STRATO - LATMOS, 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)-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), Deutscher Wetterdienst Offenbach (DWD), NASA Goddard Space Flight Center (GSFC), Finnish Meteorological Institute (FMI), DLR Institut für Physik der Atmosphäre (IPA), Deutsches Zentrum für Luft- und Raumfahrt Oberpfaffenhofen-Wessling (DLR)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2018
Subjects:
Online Access:https://insu.hal.science/insu-01661898
https://insu.hal.science/insu-01661898/document
https://insu.hal.science/insu-01661898/file/acp-18-6427-2018.pdf
https://doi.org/10.5194/acp-18-6427-2018
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institution Open Polar
collection Institut national des sciences de l'Univers: HAL-INSU
op_collection_id ftinsu
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]
Zerefos, Christos
Kapsomenakis, John
Eleftheratos, Kostas
Tourpali, Kleareti
Petropavlovskikh, Irina
Hubert, Daan
Godin-Beekmann, Sophie
Steinbrecht, Wolfgang
Frith, Stacey
Sofieva, Viktoria
Hassler, Birgit
Representativeness of single lidar stations for zonally averaged ozone profiles, their trends and attribution to proxies
topic_facet [PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph]
description International audience This paper is focusing on the representativenessof single lidar stations for zonally averaged ozone profilevariations over the middle and upper stratosphere. From thelower to the upper stratosphere, ozone profiles from singleor grouped lidar stations correlate well with zonal meanscalculated from the Solar Backscatter Ultraviolet Radiome-ter (SBUV) satellite overpasses. The best representativenesswith significant correlation coefficients is found within15of latitude circles north or south of any lidar station. Thispaper also includes a multivariate linear regression (MLR)analysis on the relative importance of proxy time series forexplaining variations in the vertical ozone profiles. Stud-ied proxies represent variability due to influences outsideof the earth system (solar cycle) and within the earth sys-tem, i.e. dynamic processes (the Quasi Biennial Oscilla-tion, QBO; the Arctic Oscillation, AO; the Antarctic Os-cillation, AAO; the El Niño Southern Oscillation, ENSO),those due to volcanic aerosol (aerosol optical depth, AOD),tropopause height changes (including global warming) andthose influences due to anthropogenic contributions to at-mospheric chemistry (equivalent effective stratospheric chlo-rine, EESC). Ozone trends are estimated, with and with-out removal of proxies, from the total available 1980 to2015 SBUV record. Except for the chemistry related proxy(EESC) and its orthogonal function, the removal of the otherproxies does not alter the significance of the estimated long-term trends. At heights above 15 hPa an “inflection point”between 1997 and 1999 marks the end of significant nega-tive ozone trends, followed by a recent period between 1998and 2015 with positive ozone trends. At heights between 15and 40 hPa the pre-1998 negative ozone trends tend to be-come less significant as we move towards 2015, below whichthe lower stratosphere ozone decline continues in agreementwith findings of recent literature
author2 Research Centre for Atmospheric Physics and Climatology Athens
Academy of Athens
Navarino Environmental Observatory (NEO)
Faculty of Geology and Geoenvironment Athens
National and Kapodistrian University of Athens (NKUA)
Laboratory of Atmospheric Physics Thessaloniki
Aristotle University of Thessaloniki
Cooperative Institute for Research in Environmental Sciences (CIRES)
University of Colorado Boulder -National Oceanic and Atmospheric Administration (NOAA)
Belgian Institute for Space Aeronomy / Institut d'Aéronomie Spatiale de Belgique (BIRA-IASB)
STRATO - LATMOS
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)-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)
Deutscher Wetterdienst Offenbach (DWD)
NASA Goddard Space Flight Center (GSFC)
Finnish Meteorological Institute (FMI)
DLR Institut für Physik der Atmosphäre (IPA)
Deutsches Zentrum für Luft- und Raumfahrt Oberpfaffenhofen-Wessling (DLR)
format Article in Journal/Newspaper
author Zerefos, Christos
Kapsomenakis, John
Eleftheratos, Kostas
Tourpali, Kleareti
Petropavlovskikh, Irina
Hubert, Daan
Godin-Beekmann, Sophie
Steinbrecht, Wolfgang
Frith, Stacey
Sofieva, Viktoria
Hassler, Birgit
author_facet Zerefos, Christos
Kapsomenakis, John
Eleftheratos, Kostas
Tourpali, Kleareti
Petropavlovskikh, Irina
Hubert, Daan
Godin-Beekmann, Sophie
Steinbrecht, Wolfgang
Frith, Stacey
Sofieva, Viktoria
Hassler, Birgit
author_sort Zerefos, Christos
title Representativeness of single lidar stations for zonally averaged ozone profiles, their trends and attribution to proxies
title_short Representativeness of single lidar stations for zonally averaged ozone profiles, their trends and attribution to proxies
title_full Representativeness of single lidar stations for zonally averaged ozone profiles, their trends and attribution to proxies
title_fullStr Representativeness of single lidar stations for zonally averaged ozone profiles, their trends and attribution to proxies
title_full_unstemmed Representativeness of single lidar stations for zonally averaged ozone profiles, their trends and attribution to proxies
title_sort representativeness of single lidar stations for zonally averaged ozone profiles, their trends and attribution to proxies
publisher HAL CCSD
publishDate 2018
url https://insu.hal.science/insu-01661898
https://insu.hal.science/insu-01661898/document
https://insu.hal.science/insu-01661898/file/acp-18-6427-2018.pdf
https://doi.org/10.5194/acp-18-6427-2018
genre Antarc*
Antarctic
Arctic
Global warming
genre_facet Antarc*
Antarctic
Arctic
Global warming
op_source ISSN: 1680-7316
EISSN: 1680-7324
Atmospheric Chemistry and Physics
https://insu.hal.science/insu-01661898
Atmospheric Chemistry and Physics, 2018, 18, pp.6427-6440. ⟨10.5194/acp-18-6427-2018⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.5194/acp-18-6427-2018
insu-01661898
https://insu.hal.science/insu-01661898
https://insu.hal.science/insu-01661898/document
https://insu.hal.science/insu-01661898/file/acp-18-6427-2018.pdf
doi:10.5194/acp-18-6427-2018
op_rights http://creativecommons.org/licenses/by/
info:eu-repo/semantics/OpenAccess
op_doi https://doi.org/10.5194/acp-18-6427-2018
container_title Atmospheric Chemistry and Physics
container_volume 18
container_issue 9
container_start_page 6427
op_container_end_page 6440
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spelling ftinsu:oai:HAL:insu-01661898v1 2023-11-05T03:33:25+01:00 Representativeness of single lidar stations for zonally averaged ozone profiles, their trends and attribution to proxies Zerefos, Christos Kapsomenakis, John Eleftheratos, Kostas Tourpali, Kleareti Petropavlovskikh, Irina Hubert, Daan Godin-Beekmann, Sophie Steinbrecht, Wolfgang Frith, Stacey Sofieva, Viktoria Hassler, Birgit Research Centre for Atmospheric Physics and Climatology Athens Academy of Athens Navarino Environmental Observatory (NEO) Faculty of Geology and Geoenvironment Athens National and Kapodistrian University of Athens (NKUA) Laboratory of Atmospheric Physics Thessaloniki Aristotle University of Thessaloniki Cooperative Institute for Research in Environmental Sciences (CIRES) University of Colorado Boulder -National Oceanic and Atmospheric Administration (NOAA) Belgian Institute for Space Aeronomy / Institut d'Aéronomie Spatiale de Belgique (BIRA-IASB) STRATO - LATMOS 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)-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) Deutscher Wetterdienst Offenbach (DWD) NASA Goddard Space Flight Center (GSFC) Finnish Meteorological Institute (FMI) DLR Institut für Physik der Atmosphäre (IPA) Deutsches Zentrum für Luft- und Raumfahrt Oberpfaffenhofen-Wessling (DLR) 2018 https://insu.hal.science/insu-01661898 https://insu.hal.science/insu-01661898/document https://insu.hal.science/insu-01661898/file/acp-18-6427-2018.pdf https://doi.org/10.5194/acp-18-6427-2018 en eng HAL CCSD European Geosciences Union info:eu-repo/semantics/altIdentifier/doi/10.5194/acp-18-6427-2018 insu-01661898 https://insu.hal.science/insu-01661898 https://insu.hal.science/insu-01661898/document https://insu.hal.science/insu-01661898/file/acp-18-6427-2018.pdf doi:10.5194/acp-18-6427-2018 http://creativecommons.org/licenses/by/ info:eu-repo/semantics/OpenAccess ISSN: 1680-7316 EISSN: 1680-7324 Atmospheric Chemistry and Physics https://insu.hal.science/insu-01661898 Atmospheric Chemistry and Physics, 2018, 18, pp.6427-6440. ⟨10.5194/acp-18-6427-2018⟩ [PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph] info:eu-repo/semantics/article Journal articles 2018 ftinsu https://doi.org/10.5194/acp-18-6427-2018 2023-10-11T16:34:43Z International audience This paper is focusing on the representativenessof single lidar stations for zonally averaged ozone profilevariations over the middle and upper stratosphere. From thelower to the upper stratosphere, ozone profiles from singleor grouped lidar stations correlate well with zonal meanscalculated from the Solar Backscatter Ultraviolet Radiome-ter (SBUV) satellite overpasses. The best representativenesswith significant correlation coefficients is found within15of latitude circles north or south of any lidar station. Thispaper also includes a multivariate linear regression (MLR)analysis on the relative importance of proxy time series forexplaining variations in the vertical ozone profiles. Stud-ied proxies represent variability due to influences outsideof the earth system (solar cycle) and within the earth sys-tem, i.e. dynamic processes (the Quasi Biennial Oscilla-tion, QBO; the Arctic Oscillation, AO; the Antarctic Os-cillation, AAO; the El Niño Southern Oscillation, ENSO),those due to volcanic aerosol (aerosol optical depth, AOD),tropopause height changes (including global warming) andthose influences due to anthropogenic contributions to at-mospheric chemistry (equivalent effective stratospheric chlo-rine, EESC). Ozone trends are estimated, with and with-out removal of proxies, from the total available 1980 to2015 SBUV record. Except for the chemistry related proxy(EESC) and its orthogonal function, the removal of the otherproxies does not alter the significance of the estimated long-term trends. At heights above 15 hPa an “inflection point”between 1997 and 1999 marks the end of significant nega-tive ozone trends, followed by a recent period between 1998and 2015 with positive ozone trends. At heights between 15and 40 hPa the pre-1998 negative ozone trends tend to be-come less significant as we move towards 2015, below whichthe lower stratosphere ozone decline continues in agreementwith findings of recent literature Article in Journal/Newspaper Antarc* Antarctic Arctic Global warming Institut national des sciences de l'Univers: HAL-INSU Atmospheric Chemistry and Physics 18 9 6427 6440