Journal articles
Seventeen years of ozone sounding at L'Aquila, Italy: evidence of mid-latitude stratospheric ozone recovery and tropospheric profile changes
Daniele Visioni
1
Giovanni Pitari
2
Vincenzo Rizi
2, 3
Marco Iarlori
2, 3
Irene Cionni
4
Ilaria Quaglia
2
Hideharu Akiyoshi
5
Slimane Bekki
6
Neal Butchart
7
Martin Chipperfield
8
Makoto Deushi
9
Sandip S. Dhomse
8
Rolando Garcia
10
Patrick Joeckel
11
Douglas Kinnison
10
Jean-François Lamarque
10
Marion Marchand
6
Martine Michou
12
Olaf Morgenstern
13
Tatsuya Nagashima
5
Fiona M. O'Connor
7
Luke Oman
14
David Plummer
15
Eugene Rozanov
16
David Saint-Martin
12
Robyn Schofield
17
John Scinocca
15
Andrea Stenke
16
Kane Stone
17
Kengo Sudo
18
Taichu Tanaka
9
Simone Tilmes
10
Holger Tost
11
Yousuke Yamashita
5
Guang Zeng
13
Daniele Visioni 1
Author
Giovanni Pitari 2
Author
Vincenzo Rizi 2, 3
Author
Marco Iarlori 2, 3
Author
Irene Cionni 4
Author
Ilaria Quaglia 2
Author
Hideharu Akiyoshi 5
Author
Slimane Bekki 6
Author IdHAL : slimane-bekki ResearcherId : http://www.researcherid.com/rid/J-7221-2015 ORCID : https://orcid.org/0000-0002-5538-0800
Neal Butchart 7
Author
Martin Chipperfield 8
Author
Makoto Deushi 9
Author
Sandip S. Dhomse 8
Author
Rolando Garcia 10
Author
Patrick Joeckel 11
Author
Douglas Kinnison 10
Author
Jean-François Lamarque 10
Author
Marion Marchand 6
Author IdHAL : marion-marchand IdRef : https://www.idref.fr/070160856 ORCID : https://orcid.org/0000-0003-2220-383X VIAF : http://viaf.org/viaf/210030347 ISNI : http://isni.org/isni/0000000432000283
Martine Michou 12
Author
Olaf Morgenstern 13
Author
Tatsuya Nagashima 5
Author
David Saint-Martin 12
Author
Robyn Schofield 17
Author
John Scinocca 15
Author
Andrea Stenke 16
Author
1
MAE - Sibley School of Mechanical and Aerospace Engineering ( Ithaca, New York 14853 - United States)
- Cornell University ( Ithaca, New York 14853 - United States)
2
DSFC - Department of Physical and Chemical Sciences [L'Aquila] (Italy)
- UNIVAQ - Università degli Studi dell'Aquila (Via Giovanni Di Vincenzo 16/B, 67100 L'Aquila - Italy)
3
Centre of Excellence CETEMPS (Via Vetoio (Coppito 1), 67100 Coppito (AQ) - Italy)
- UNIVAQ - Università degli Studi dell'Aquila (Via Giovanni Di Vincenzo 16/B, 67100 L'Aquila - Italy)
4
ENEA - Agenzia Nazionale per le nuove Tecnologie, l’energia e lo sviluppo economico sostenibile (Lungotevere Thaon di Revel, 76 - 00196 ROMA - Italy)
5
NIES - National Institute for Environmental Studies (Tsukuba, Ibaraki - Japan)
6
STRATO - LATMOS (France)
- LATMOS - Laboratoire Atmosphères, Milieux, Observations Spatiales (11 boulevard d'Alembert
Quartier des Garennes
78280 - Guyancourt - France)
- SU - Sorbonne Université : UMR8190 (21 rue de l’École de médecine - 75006 Paris - France)
- UVSQ - Université de Versailles Saint-Quentin-en-Yvelines : UMR8190 (55 avenue de Paris - 78035 Versailles cedex - France)
- CNRS - Centre National de la Recherche Scientifique : UMR8190 (France)
- INSU - CNRS - Institut national des sciences de l'Univers : UMR8190 (INSU-CNRS 3 rue Michel-Ange, 75794 Paris Cedex 16 - France)
7
MOHC - Met Office Hadley Centre (Exeter - United Kingdom)
- United Kingdom Met Office [Exeter] (FitzRoy Road, Exeter, Devon, EX1 3PB, UK - United Kingdom)
8
SEE - School of Earth and Environment [Leeds] (Maths/Earth and Environment Building, The University of Leeds, Leeds. LS2 9JT - United Kingdom)
- University of Leeds (Woodhouse Lane, Leeds LS2 9JT - United Kingdom)
9
MRI - Meteorological Research Institute [Tsukuba] (1-1 Nagamine, Tsukuba, Ibaraki 305-0052, Japan - Japan)
- JMA - Japan Meteorological Agency (1-3-4 Otemachi, Chiyoda-ku, Tokyo 100-8122, Japan - Japan)
10
NCAR - National Center for Atmospheric Research [Boulder] (3090 Center Green Drive, Boulder, CO 80301 - United States)
11
IPA - DLR Institut für Physik der Atmosphäre (Oberpfaffenhofen-Wessling - Germany)
- DLR - Deutsches Zentrum für Luft- und Raumfahrt [Oberpfaffenhofen-Wessling] (Münchener Straße 20, 82234 Weßling - Germany)
12
CNRM - Centre national de recherches météorologiques (France)
- CNRS - Centre National de la Recherche Scientifique : UMR3589 (France)
- Météo France (France)
13
NIWA - National Institute of Water and Atmospheric Research [Wellington] (301 Evans Bay Parade, Hataitai, Wellington 6021 - New Zealand)
14
GSFC - NASA Goddard Space Flight Center (Greenbelt, MD 20771 - United States)
15
Environment and Climate Change Canada (Gatineau, Québec - Canada)
16
IAC - Institute for Atmospheric and Climate Science [Zürich] (8092 Zürich - Switzerland)
- ETH Zürich - Eidgenössische Technische Hochschule - Swiss Federal Institute of Technology in Zürich [Zürich] (Hauptgebäude, Rämistrasse 101, 8092 Zürich - Switzerland)
17
School of Earth Sciences [Melbourne] (Parkville, VIC Australia 3010 - Australia)
- Faculty of Science [Melbourne] ( Building 155, The University of Melbourne, Masson Rd, Melbourne VIC 3052, Australia - Australia)
- University of Melbourne (Parkville VIC 3010 - Australia)
18
Graduate School of Environmental Studies [Nagoya] ( Furo-cho, Chikusa-ku, Nagoya, Japan 464-8601 - Japan)
- Nagoya University (1 Furocho, Chikusa Ward, Nagoya, Aichi Prefecture 464-0814, Japon - Japan)
Abstract : Ozone profile measurements collected at L'Aquila (Italy, 42.4°N) during seventeen years of radio-sounding 30 (2000-2016) are presented here, with an analysis of derived trends. Model results from the SPARC-CCMI exercise are used in parallel to highlight the physical and chemical mechanisms regulating mid-latitude ozone trends. The statistically significant trends highlighted in time series at L'Aquila are those in the mid-upper stratosphere (+5.9±4.2), mid troposphere https://doi.org/10.5194/acp-2020-525 Preprint. Discussion started: 1 July 2020 c Author(s) 2020. CC BY 4.0 License. 2 (+5.9±2.4) and upper troposphere (+2.5±0.9), all in percent/decade. The upper stratospheric positive trend was already well documented in recent WMO assessments and attributed to the starting decline of stratospheric Cly and Bry and to the 35 stratospheric cooling induced by increasing well mixed greenhouse gases, thus slowing down gas-phase reactions that destroy ozone in the upper stratosphere. The ozone increase in the mid-upper troposphere is largely regulated by the increasing strength of the Brewer-Dobson circulation, which moves more ozone from the tropics to the extratropics and enhances the tropospheric influx from the lowermost stratosphere. This climate feedback mechanism on tropospheric ozone is only partially compensated by the increasing chemical ozone loss associated to higher H2O values in response to the 40 tropospheric warming. We also note that ozone trends obtained in the lower stratosphere are negative (-2.2 percent/decade), but do not result to be statistically significant in our analyses.
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Journal articles
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https://hal-insu.archives-ouvertes.fr/insu-02886950
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Submitted on : Monday, December 7, 2020 - 9:34:35 AM
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Contributor : Catherine Cardon <>
Submitted on : Monday, December 7, 2020 - 9:34:35 AM
Last modification on : Saturday, December 12, 2020 - 12:10:12 PM
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- HAL Id : insu-02886950, version 1
- DOI : 10.5194/acp-2020-525
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INSU | SU-SCIENCES | SORBONNE-UNIVERSITE | UVSQ | LATMOS | CNRS | METEO | SU-TI
Citation
Daniele Visioni, Giovanni Pitari, Vincenzo Rizi, Marco Iarlori, Irene Cionni, et al.. Seventeen years of ozone sounding at L'Aquila, Italy: evidence of mid-latitude stratospheric ozone recovery and tropospheric profile changes. Atmospheric Chemistry and Physics Discussions, European Geosciences Union, 2020, pp.(Under Review). ⟨10.5194/acp-2020-525⟩. ⟨insu-02886950⟩
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