Estimation of Antarctic ozone loss from ground-based total column measurements

International audience The passive tracer method is used to estimate ozone loss from ground-based measurements in the Antarctic. A sensitivity study shows that the ozone depletion can be estimated within an accuracy of ~4%. The method is then applied to the ground-based observations from Arrival Hei...

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Published in:Atmospheric Chemistry and Physics
Main Authors: Kuttippurath, Jayanarayanan, Goutail, Florence, Pommereau, Jean-Pierre, Lefèvre, Franck, Roscoe, H. K., Pazmino, Andrea, Feng, W., Chipperfield, M. P., Godin-Beekmann, Sophie
Other Authors: 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), British Antarctic Survey (BAS), Natural Environment Research Council (NERC), School of Earth and Environment Leeds (SEE), University of Leeds
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2010
Subjects:
Online Access:https://hal.science/hal-00469607
https://hal.science/hal-00469607/document
https://hal.science/hal-00469607/file/acp-10-6569-2010.pdf
https://doi.org/10.5194/acp-10-6569-2010
id ftinsu:oai:HAL:hal-00469607v1
record_format openpolar
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]
Kuttippurath, Jayanarayanan
Goutail, Florence
Pommereau, Jean-Pierre
Lefèvre, Franck
Roscoe, H. K.
Pazmino, Andrea
Feng, W.
Chipperfield, M. P.
Godin-Beekmann, Sophie
Estimation of Antarctic ozone loss from ground-based total column measurements
topic_facet [PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph]
description International audience The passive tracer method is used to estimate ozone loss from ground-based measurements in the Antarctic. A sensitivity study shows that the ozone depletion can be estimated within an accuracy of ~4%. The method is then applied to the ground-based observations from Arrival Heights, Belgrano, Concordia, Dumont d'Urville, Faraday, Halley, Marambio, Neumayer, Rothera, South Pole, Syowa, and Zhongshan for the diagnosis of ozone loss in the Antarctic. On average, the ten-day boxcar average of the vortex mean ozone column loss deduced from the ground-based stations was about 55±5% in 2005-2009. The ozone loss computed from the ground-based measurements is in very good agreement with those derived from satellite measurements (OMI and SCIAMACHY) and model simulations (REPROBUS and SLIMCAT), where the differences are within ±3-5%. The historical ground-based total ozone observations in October show that the depletion started in the late 1970s, reached a maximum in the early 1990s and stabilised afterwards due to saturation. There is no indication of ozone recovery yet. At southern mid-latitudes, a reduction of 20-50% is observed for a few days in October-November at the newly installed Rio Gallegos station. Similar depletion of ozone is also observed episodically during the vortex overpasses at Kerguelen in October-November and at Macquarie Island in July-August of the recent winters. This illustrates the significance of measurements at the edges of Antarctica.
author2 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)
British Antarctic Survey (BAS)
Natural Environment Research Council (NERC)
School of Earth and Environment Leeds (SEE)
University of Leeds
format Article in Journal/Newspaper
author Kuttippurath, Jayanarayanan
Goutail, Florence
Pommereau, Jean-Pierre
Lefèvre, Franck
Roscoe, H. K.
Pazmino, Andrea
Feng, W.
Chipperfield, M. P.
Godin-Beekmann, Sophie
author_facet Kuttippurath, Jayanarayanan
Goutail, Florence
Pommereau, Jean-Pierre
Lefèvre, Franck
Roscoe, H. K.
Pazmino, Andrea
Feng, W.
Chipperfield, M. P.
Godin-Beekmann, Sophie
author_sort Kuttippurath, Jayanarayanan
title Estimation of Antarctic ozone loss from ground-based total column measurements
title_short Estimation of Antarctic ozone loss from ground-based total column measurements
title_full Estimation of Antarctic ozone loss from ground-based total column measurements
title_fullStr Estimation of Antarctic ozone loss from ground-based total column measurements
title_full_unstemmed Estimation of Antarctic ozone loss from ground-based total column measurements
title_sort estimation of antarctic ozone loss from ground-based total column measurements
publisher HAL CCSD
publishDate 2010
url https://hal.science/hal-00469607
https://hal.science/hal-00469607/document
https://hal.science/hal-00469607/file/acp-10-6569-2010.pdf
https://doi.org/10.5194/acp-10-6569-2010
long_lat ENVELOPE(140.017,140.017,-66.667,-66.667)
ENVELOPE(140.013,140.013,-66.667,-66.667)
ENVELOPE(-68.130,-68.130,-67.568,-67.568)
ENVELOPE(-64.256,-64.256,-65.246,-65.246)
ENVELOPE(-56.750,-56.750,-64.283,-64.283)
ENVELOPE(76.371,76.371,-69.373,-69.373)
ENVELOPE(-67.150,-67.150,-68.133,-68.133)
ENVELOPE(166.650,166.650,-77.817,-77.817)
ENVELOPE(-64.967,-64.967,-65.150,-65.150)
geographic Antarctic
The Antarctic
Kerguelen
Neumayer
South Pole
Dumont d'Urville
Dumont-d'Urville
Rothera
Faraday
Marambio
Zhongshan
Gallegos
Arrival Heights
Belgrano
geographic_facet Antarctic
The Antarctic
Kerguelen
Neumayer
South Pole
Dumont d'Urville
Dumont-d'Urville
Rothera
Faraday
Marambio
Zhongshan
Gallegos
Arrival Heights
Belgrano
genre Antarc*
Antarctic
Antarctica
Macquarie Island
South pole
South pole
genre_facet Antarc*
Antarctic
Antarctica
Macquarie Island
South pole
South pole
op_source ISSN: 1680-7316
EISSN: 1680-7324
Atmospheric Chemistry and Physics
https://hal.science/hal-00469607
Atmospheric Chemistry and Physics, 2010, 10 (14), pp.6569-6581. ⟨10.5194/acp-10-6569-2010⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.5194/acp-10-6569-2010
hal-00469607
https://hal.science/hal-00469607
https://hal.science/hal-00469607/document
https://hal.science/hal-00469607/file/acp-10-6569-2010.pdf
doi:10.5194/acp-10-6569-2010
op_rights info:eu-repo/semantics/OpenAccess
op_doi https://doi.org/10.5194/acp-10-6569-2010
container_title Atmospheric Chemistry and Physics
container_volume 10
container_issue 14
container_start_page 6569
op_container_end_page 6581
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spelling ftinsu:oai:HAL:hal-00469607v1 2023-06-18T03:38:05+02:00 Estimation of Antarctic ozone loss from ground-based total column measurements Kuttippurath, Jayanarayanan Goutail, Florence Pommereau, Jean-Pierre Lefèvre, Franck Roscoe, H. K. Pazmino, Andrea Feng, W. Chipperfield, M. P. Godin-Beekmann, Sophie 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) British Antarctic Survey (BAS) Natural Environment Research Council (NERC) School of Earth and Environment Leeds (SEE) University of Leeds 2010 https://hal.science/hal-00469607 https://hal.science/hal-00469607/document https://hal.science/hal-00469607/file/acp-10-6569-2010.pdf https://doi.org/10.5194/acp-10-6569-2010 en eng HAL CCSD European Geosciences Union info:eu-repo/semantics/altIdentifier/doi/10.5194/acp-10-6569-2010 hal-00469607 https://hal.science/hal-00469607 https://hal.science/hal-00469607/document https://hal.science/hal-00469607/file/acp-10-6569-2010.pdf doi:10.5194/acp-10-6569-2010 info:eu-repo/semantics/OpenAccess ISSN: 1680-7316 EISSN: 1680-7324 Atmospheric Chemistry and Physics https://hal.science/hal-00469607 Atmospheric Chemistry and Physics, 2010, 10 (14), pp.6569-6581. ⟨10.5194/acp-10-6569-2010⟩ [PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph] info:eu-repo/semantics/article Journal articles 2010 ftinsu https://doi.org/10.5194/acp-10-6569-2010 2023-06-06T01:17:36Z International audience The passive tracer method is used to estimate ozone loss from ground-based measurements in the Antarctic. A sensitivity study shows that the ozone depletion can be estimated within an accuracy of ~4%. The method is then applied to the ground-based observations from Arrival Heights, Belgrano, Concordia, Dumont d'Urville, Faraday, Halley, Marambio, Neumayer, Rothera, South Pole, Syowa, and Zhongshan for the diagnosis of ozone loss in the Antarctic. On average, the ten-day boxcar average of the vortex mean ozone column loss deduced from the ground-based stations was about 55±5% in 2005-2009. The ozone loss computed from the ground-based measurements is in very good agreement with those derived from satellite measurements (OMI and SCIAMACHY) and model simulations (REPROBUS and SLIMCAT), where the differences are within ±3-5%. The historical ground-based total ozone observations in October show that the depletion started in the late 1970s, reached a maximum in the early 1990s and stabilised afterwards due to saturation. There is no indication of ozone recovery yet. At southern mid-latitudes, a reduction of 20-50% is observed for a few days in October-November at the newly installed Rio Gallegos station. Similar depletion of ozone is also observed episodically during the vortex overpasses at Kerguelen in October-November and at Macquarie Island in July-August of the recent winters. This illustrates the significance of measurements at the edges of Antarctica. Article in Journal/Newspaper Antarc* Antarctic Antarctica Macquarie Island South pole South pole Institut national des sciences de l'Univers: HAL-INSU Antarctic The Antarctic Kerguelen Neumayer South Pole Dumont d'Urville ENVELOPE(140.017,140.017,-66.667,-66.667) Dumont-d'Urville ENVELOPE(140.013,140.013,-66.667,-66.667) Rothera ENVELOPE(-68.130,-68.130,-67.568,-67.568) Faraday ENVELOPE(-64.256,-64.256,-65.246,-65.246) Marambio ENVELOPE(-56.750,-56.750,-64.283,-64.283) Zhongshan ENVELOPE(76.371,76.371,-69.373,-69.373) Gallegos ENVELOPE(-67.150,-67.150,-68.133,-68.133) Arrival Heights ENVELOPE(166.650,166.650,-77.817,-77.817) Belgrano ENVELOPE(-64.967,-64.967,-65.150,-65.150) Atmospheric Chemistry and Physics 10 14 6569 6581