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Trends of Studies on Controlled Halogenated Gases under International Conventions during 1999–2018 Using Bibliometric Analysis: A Global Perspective. SUSTAINABILITY 2022. [DOI: 10.3390/su14020806] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 12/04/2022]
Abstract
A lot of research on international convention-controlled halogenated gases (CHGs) has been carried out. However, few bibliometric analyses and literature reviews exist in this field. Based on 734 articles extracted from the Science Citation Index (SCI) Expanded database of the Web of Science, we provided the visualisation for the performance of contributors and trends in research content by using VOSviewer and Science of Science (Sci2). The results showed that the United States was the most productive country, followed by the United Kingdom and China. The National Oceanic and Atmospheric Administration had the largest number of publications, followed by the Massachusetts Institute of Technology (MIT) and the University of Bristol. In terms of disciplines, environmental science and meteorological and atmospheric science have contributed the most. By using cluster analysis of all keywords, four key research topics of CHGs were identified and reviewed: (1) emissions calculation, (2) physicochemical analysis of halocarbons, (3) evaluation of replacements, and (4) environmental impact. The change in research substances is closely related to the phase-out schedule of the Montreal Protocol. In terms of environmental impact, global warming has always been the most important research hotspot, whereas research on ozone-depleting substances and biological toxicity shows a gradually rising trend.
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2
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Chiodo G, Polvani L, Marsh D, Stenke A, Ball W, Rozanov E, Muthers S, Tsigaridis K. The response of the ozone layer to quadrupled CO 2 concentrations. JOURNAL OF CLIMATE 2019; 32:7629-7642. [PMID: 33132515 PMCID: PMC7592696 DOI: 10.1175/jcli-d-19-0086.1] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 06/11/2023]
Abstract
An accurate quantification of the stratospheric ozone feedback in climate change simulations requires knowledge of the ozone response to increased greenhouse gases. Here, we present an analysis of the ozone layer response to an abrupt quadrupling of CO2 concentrations in four chemistry-climate models. We show that increased CO2 levels lead to a decrease in ozone concentrations in the tropical lower stratosphere, and an increase over the high latitudes and throughout the upper stratosphere. This pattern is robust across all models examined here, although important inter-model differences in the magnitude of the response are found. As a result of the cancellation between upper and lower stratospheric ozone, the total column ozone response in the tropics is small, and appears to be model dependent. A substantial portion of the spread in the tropical column ozone is tied to inter-model spread in upwelling. The high latitude ozone response is strongly seasonally dependent, and shows increases peaking in late-winter and spring of each hemisphere, with prominent longitudinal asymmetries. The range of ozone responses to CO2 reported in this paper has the potential to induce significant radiative and dynamical effects on the simulated climate. Hence, these results highlight the need of using an ozone dataset consistent with CO2 forcing in models involved in climate sensitivity studies.
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Affiliation(s)
- G. Chiodo
- Department of Applied Physics and Applied Mathematics, Columbia University, New York, NY, USA
| | - L.M. Polvani
- Department of Applied Physics and Applied Mathematics, Columbia University, New York, NY, USA
| | - D.R. Marsh
- National Center for Atmospheric Research, Boulder, CO, USA
| | | | - W. Ball
- Physikalisch-Metorologisches Observatorium Davos - World Radiation Center, Davos, Switzerland, and IAC ETH, Zrich, Switzerland
| | - E. Rozanov
- Physikalisch-Metorologisches Observatorium Davos - World Radiation Center, Davos, Switzerland, and IAC ETH, Zrich, Switzerland
| | - S. Muthers
- Deutscher Wetterdienst, Research Center Human Biometeorology, Freiburg 79104, Germany
| | - K. Tsigaridis
- Center for Climate Systems Research, Columbia University, and NASA Goddard Institute for Space Studies, New York, NY, USA
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3
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Wargan K, Orbe C, Pawson S, Ziemke JR, Oman LD, Olsen MA, Coy L, Knowland KE. Recent decline in extratropical lower stratospheric ozone attributed to circulation changes. GEOPHYSICAL RESEARCH LETTERS 2018; 45:5166-5176. [PMID: 30381777 PMCID: PMC6204267 DOI: 10.1029/2018gl077406] [Citation(s) in RCA: 5] [Impact Index Per Article: 0.8] [Reference Citation Analysis] [Abstract] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 01/31/2018] [Accepted: 05/06/2018] [Indexed: 06/08/2023]
Abstract
1998-2016 ozone trends in the lower stratosphere (LS) are examined using the Modern-Era Retrospective Analysis for Research and Applications Version 2 (MERRA-2) and related NASA products. After removing biases resulting from step-changes in the MERRA-2 ozone observations, a discernible negative trend of -1.67±0.54 Dobson units per decade (DU/decade) is found in the 10-km layer above the tropopause between 20°N and 60°N. A weaker but statistically significant trend of -1.17±0.33 DU/decade exists between 50°S and 20°S. In the Tropics, a positive trend is seen in a 5-km layer above the tropopause. Analysis of an idealized tracer in a model simulation constrained by MERRA-2 meteorological fields provides strong evidence that these trends are driven by enhanced isentropic transport between the tropical (20°S-20°N) and extratropical LS in the past two decades. This is the first time that a reanalysis dataset has been used to detect and attribute trends in lower stratospheric ozone.
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Affiliation(s)
- Krzysztof Wargan
- Science Systems and Applications Inc., Lanham, Maryland, USA
- Global Modeling and Assimilation Office, Code 610.1, NASA Goddard Space Flight Center, Greenbelt, Maryland, USA
| | - Clara Orbe
- Code 611, NASA Goddard Institute for Space Studies, New York, NY, USA
| | - Steven Pawson
- Global Modeling and Assimilation Office, Code 610.1, NASA Goddard Space Flight Center, Greenbelt, Maryland, USA
| | - Jerald R. Ziemke
- Goddard Earth Science Technology & Research (GESTAR) Morgan State University, Baltimore, MD USA
- Atmospheric Chemistry and Dynamics Laboratory, Code 614, NASA Goddard Space Flight Center, Greenbelt, Maryland, USA
| | - Luke D. Oman
- Atmospheric Chemistry and Dynamics Laboratory, Code 614, NASA Goddard Space Flight Center, Greenbelt, Maryland, USA
| | - Mark A. Olsen
- Goddard Earth Science Technology & Research (GESTAR) Morgan State University, Baltimore, MD USA
- Atmospheric Chemistry and Dynamics Laboratory, Code 614, NASA Goddard Space Flight Center, Greenbelt, Maryland, USA
| | - Lawrence Coy
- Science Systems and Applications Inc., Lanham, Maryland, USA
- Global Modeling and Assimilation Office, Code 610.1, NASA Goddard Space Flight Center, Greenbelt, Maryland, USA
| | - K. Emma Knowland
- Global Modeling and Assimilation Office, Code 610.1, NASA Goddard Space Flight Center, Greenbelt, Maryland, USA
- Goddard Earth Science Technology & Research (GESTAR), Universities Space Research Association (USRA), Columbia, MD USA
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Hubert D, Lambert JC, Verhoelst T, Granville J, Keppens A, Baray JL, Cortesi U, Degenstein DA, Froidevaux L, Godin-Beekmann S, Hoppel KW, Kyrölä E, Leblanc T, Lichtenberg G, McElroy CT, Murtagh D, Nakane H, Querel R, Russell JM, Salvador J, Smit HGJ, Stebel K, Steinbrecht W, Strawbridge KB, Stübi R, Swart DPJ, Taha G, Thompson AM, Urban J, van Gijsel JAE, von der Gathen P, Walker KA, Wolfram E, Zawodny JM. Ground-based assessment of the bias and long-term stability of fourteen limb and occultation ozone profile data records. ATMOSPHERIC MEASUREMENT TECHNIQUES 2016; 9:2497-2534. [PMID: 29743958 PMCID: PMC5937289 DOI: 10.5194/amtd-8-6661-2015] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 06/08/2023]
Abstract
The ozone profile records of a large number of limb and occultation satellite instruments are widely used to address several key questions in ozone research. Further progress in some domains depends on a more detailed understanding of these data sets, especially of their long-term stability and their mutual consistency. To this end, we made a systematic assessment of fourteen limb and occultation sounders that, together, provide more than three decades of global ozone profile measurements. In particular, we considered the latest operational Level-2 records by SAGE II, SAGE III, HALOE, UARS MLS, Aura MLS, POAM II, POAM III, OSIRIS, SMR, GOMOS, MIPAS, SCIAMACHY, ACE-FTS and MAESTRO. Central to our work is a consistent and robust analysis of the comparisons against the ground-based ozonesonde and stratospheric ozone lidar networks. It allowed us to investigate, from the troposphere up to the stratopause, the following main aspects of satellite data quality: long-term stability, overall bias, and short-term variability, together with their dependence on geophysical parameters and profile representation. In addition, it permitted us to quantify the overall consistency between the ozone profilers. Generally, we found that between 20-40 km the satellite ozone measurement biases are smaller than ±5 %, the short-term variabilities are less than 5-12% and the drifts are at most ±5% decade-1 (or even ±3 % decade-1 for a few records). The agreement with ground-based data degrades somewhat towards the stratopause and especially towards the tropopause where natural variability and low ozone abundances impede a more precise analysis. In part of the stratosphere a few records deviate from the preceding general conclusions; we identified biases of 10% and more (POAM II and SCIAMACHY), markedly higher single-profile variability (SMR and SCIAMACHY), and significant long-term drifts (SCIAMACHY, OSIRIS, HALOE, and possibly GOMOS and SMR as well). Furthermore, we reflected on the repercussions of our findings for the construction, analysis and interpretation of merged data records. Most notably, the discrepancies between several recent ozone profile trend assessments can be mostly explained by instrumental drift. This clearly demonstrates the need for systematic comprehensive multi-instrument comparison analyses.
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Affiliation(s)
- D. Hubert
- Royal Belgian Institute for Space Aeronomy (BIRA-IASB), Brussels,
Belgium
| | - J.-C. Lambert
- Royal Belgian Institute for Space Aeronomy (BIRA-IASB), Brussels,
Belgium
| | - T. Verhoelst
- Royal Belgian Institute for Space Aeronomy (BIRA-IASB), Brussels,
Belgium
| | - J. Granville
- Royal Belgian Institute for Space Aeronomy (BIRA-IASB), Brussels,
Belgium
| | - A. Keppens
- Royal Belgian Institute for Space Aeronomy (BIRA-IASB), Brussels,
Belgium
| | - J.-L. Baray
- Laboratoire de l’Atmosphère et des Cyclones
(Université de La Réunion, CNRS, Météo-France),
OSU-Réunion (Université de la Réunion, CNRS), La
Réunion, France
- Laboratoire de Météorologie Physique, Observatoire
de Physique du Globe de Clermont-Ferrand (Université Blaise Pascal, CNRS),
Clermont-Ferrand, France
| | - U. Cortesi
- Istituto di Fisica Applicata “Nello Carrara” del
Consiglio Nazionale delle Ricerche, Sesto Fiorentino, Italy
| | - D. A. Degenstein
- Institute of Space and Atmospheric Studies, University of
Saskatchewan, Saskatoon, SK, Canada
| | - L. Froidevaux
- Jet Propulsion Laboratory, California Institute of Technology,
Pasadena, CA, USA
| | - S. Godin-Beekmann
- Laboratoire Atmosphère Milieux Observations Spatiales,
Université de Versailles Saint-Quentin en Yvelines, Centre National de la
Recherche Scientifique, Paris, France
| | | | - E. Kyrölä
- Finnish Meteorological Institute, Helsinki, Finland
| | - T. Leblanc
- Jet Propulsion Laboratory, California Institute of Technology,
Wrightwood, CA, USA
| | - G. Lichtenberg
- German Aerospace Center (DLR), Remote Sensing Technology Institute,
Oberpfaffenhofen, Germany
| | | | - D. Murtagh
- Department of Earth and Space Sciences, Chalmers University of
Technology, Göteborg, Sweden
| | - H. Nakane
- Kochi University of Technology, Kochi, Japan
- National Institute for Environmental Studies, Tsukuba, Ibaraki,
Japan
| | - R. Querel
- National Institute of Water and Atmospheric Research, Lauder, New
Zealand
| | - J. M. Russell
- Department of Atmospheric and Planetary Science, Hampton
University, VA, USA
| | - J. Salvador
- CEILAP-UNIDEF (MINDEF-CONICET), UMI-IFAECI-CNRS-3351, Villa
Martelli, Argentina
| | - H. G. J. Smit
- Research Centre Jülich, Institute for Energy and Climate
Research: Troposphere (IEK-8), Jülich, Germany
| | - K. Stebel
- Norwegian Air Research Institute (NILU), Kjeller, Norway
| | - W. Steinbrecht
- Meteorologisches Observatorium, Deutscher Wetterdienst,
Hohenpeissenberg, Germany
| | - K. B. Strawbridge
- Air Quality Processes Research Section, Environment Canada,
Toronto, ON, Canada
| | - R. Stübi
- Payerne Aerological Station, MeteoSwiss, Payerne, Switzerland
| | - D. P. J. Swart
- National Institute for Public Health and the Environment (RIVM),
Bilthoven, the Netherlands
| | - G. Taha
- Universities Space Research Association, Greenbelt, MD, USA
- NASA Goddard Space Flight Center, Greenbelt, MD, USA
| | | | - J. Urban
- Department of Earth and Space Sciences, Chalmers University of
Technology, Göteborg, Sweden
| | | | - P. von der Gathen
- Alfred Wegener Institute, Helmholtz Centre for Polar and Marine
Research, Potsdam, Germany
| | - K. A. Walker
- Department of Physics, University of Toronto, Toronto, ON,
Canada
- Department of Chemistry, University of Waterloo, Waterloo, ON,
Canada
| | - E. Wolfram
- CEILAP-UNIDEF (MINDEF-CONICET), UMI-IFAECI-CNRS-3351, Villa
Martelli, Argentina
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5
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Hubert D, Lambert JC, Verhoelst T, Granville J, Keppens A, Baray JL, Cortesi U, Degenstein DA, Froidevaux L, Godin-Beekmann S, Hoppel KW, Kyrölä E, Leblanc T, Lichtenberg G, McElroy CT, Murtagh D, Nakane H, Querel R, Russell JM, Salvador J, Smit HGJ, Stebel K, Steinbrecht W, Strawbridge KB, Stübi R, Swart DPJ, Taha G, Thompson AM, Urban J, van Gijsel JAE, von der Gathen P, Walker KA, Wolfram E, Zawodny JM. Ground-based assessment of the bias and long-term stability of fourteen limb and occultation ozone profile data records. ATMOSPHERIC MEASUREMENT TECHNIQUES 2016; 9:2497-2534. [PMID: 29743958 DOI: 10.5194/amt-9-2497-2016] [Citation(s) in RCA: 3] [Impact Index Per Article: 0.4] [Reference Citation Analysis] [Abstract] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 05/25/2023]
Abstract
The ozone profile records of a large number of limb and occultation satellite instruments are widely used to address several key questions in ozone research. Further progress in some domains depends on a more detailed understanding of these data sets, especially of their long-term stability and their mutual consistency. To this end, we made a systematic assessment of fourteen limb and occultation sounders that, together, provide more than three decades of global ozone profile measurements. In particular, we considered the latest operational Level-2 records by SAGE II, SAGE III, HALOE, UARS MLS, Aura MLS, POAM II, POAM III, OSIRIS, SMR, GOMOS, MIPAS, SCIAMACHY, ACE-FTS and MAESTRO. Central to our work is a consistent and robust analysis of the comparisons against the ground-based ozonesonde and stratospheric ozone lidar networks. It allowed us to investigate, from the troposphere up to the stratopause, the following main aspects of satellite data quality: long-term stability, overall bias, and short-term variability, together with their dependence on geophysical parameters and profile representation. In addition, it permitted us to quantify the overall consistency between the ozone profilers. Generally, we found that between 20-40 km the satellite ozone measurement biases are smaller than ±5 %, the short-term variabilities are less than 5-12% and the drifts are at most ±5% decade-1 (or even ±3 % decade-1 for a few records). The agreement with ground-based data degrades somewhat towards the stratopause and especially towards the tropopause where natural variability and low ozone abundances impede a more precise analysis. In part of the stratosphere a few records deviate from the preceding general conclusions; we identified biases of 10% and more (POAM II and SCIAMACHY), markedly higher single-profile variability (SMR and SCIAMACHY), and significant long-term drifts (SCIAMACHY, OSIRIS, HALOE, and possibly GOMOS and SMR as well). Furthermore, we reflected on the repercussions of our findings for the construction, analysis and interpretation of merged data records. Most notably, the discrepancies between several recent ozone profile trend assessments can be mostly explained by instrumental drift. This clearly demonstrates the need for systematic comprehensive multi-instrument comparison analyses.
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Affiliation(s)
- D Hubert
- Royal Belgian Institute for Space Aeronomy (BIRA-IASB), Brussels, Belgium
| | - J-C Lambert
- Royal Belgian Institute for Space Aeronomy (BIRA-IASB), Brussels, Belgium
| | - T Verhoelst
- Royal Belgian Institute for Space Aeronomy (BIRA-IASB), Brussels, Belgium
| | - J Granville
- Royal Belgian Institute for Space Aeronomy (BIRA-IASB), Brussels, Belgium
| | - A Keppens
- Royal Belgian Institute for Space Aeronomy (BIRA-IASB), Brussels, Belgium
| | - J-L Baray
- Laboratoire de l'Atmosphère et des Cyclones (Université de La Réunion, CNRS, Météo-France), OSU-Réunion (Université de la Réunion, CNRS), La Réunion, France
- Laboratoire de Météorologie Physique, Observatoire de Physique du Globe de Clermont-Ferrand (Université Blaise Pascal, CNRS), Clermont-Ferrand, France
| | - U Cortesi
- Istituto di Fisica Applicata "Nello Carrara" del Consiglio Nazionale delle Ricerche, Sesto Fiorentino, Italy
| | - D A Degenstein
- Institute of Space and Atmospheric Studies, University of Saskatchewan, Saskatoon, SK, Canada
| | - L Froidevaux
- Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA, USA
| | - S Godin-Beekmann
- Laboratoire Atmosphère Milieux Observations Spatiales, Université de Versailles Saint-Quentin en Yvelines, Centre National de la Recherche Scientifique, Paris, France
| | | | - E Kyrölä
- Finnish Meteorological Institute, Helsinki, Finland
| | - T Leblanc
- Jet Propulsion Laboratory, California Institute of Technology, Wrightwood, CA, USA
| | - G Lichtenberg
- German Aerospace Center (DLR), Remote Sensing Technology Institute, Oberpfaffenhofen, Germany
| | | | - D Murtagh
- Department of Earth and Space Sciences, Chalmers University of Technology, Göteborg, Sweden
| | - H Nakane
- Kochi University of Technology, Kochi, Japan
- National Institute for Environmental Studies, Tsukuba, Ibaraki, Japan
| | - R Querel
- National Institute of Water and Atmospheric Research, Lauder, New Zealand
| | - J M Russell
- Department of Atmospheric and Planetary Science, Hampton University, VA, USA
| | - J Salvador
- CEILAP-UNIDEF (MINDEF-CONICET), UMI-IFAECI-CNRS-3351, Villa Martelli, Argentina
| | - H G J Smit
- Research Centre Jülich, Institute for Energy and Climate Research: Troposphere (IEK-8), Jülich, Germany
| | - K Stebel
- Norwegian Air Research Institute (NILU), Kjeller, Norway
| | - W Steinbrecht
- Meteorologisches Observatorium, Deutscher Wetterdienst, Hohenpeissenberg, Germany
| | - K B Strawbridge
- Air Quality Processes Research Section, Environment Canada, Toronto, ON, Canada
| | - R Stübi
- Payerne Aerological Station, MeteoSwiss, Payerne, Switzerland
| | - D P J Swart
- National Institute for Public Health and the Environment (RIVM), Bilthoven, the Netherlands
| | - G Taha
- Universities Space Research Association, Greenbelt, MD, USA
- NASA Goddard Space Flight Center, Greenbelt, MD, USA
| | - A M Thompson
- NASA Goddard Space Flight Center, Greenbelt, MD, USA
| | - J Urban
- Department of Earth and Space Sciences, Chalmers University of Technology, Göteborg, Sweden
| | - J A E van Gijsel
- Royal Netherlands Meteorological Institute (KNMI), De Bilt, the Netherlands
| | - P von der Gathen
- Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Potsdam, Germany
| | - K A Walker
- Department of Physics, University of Toronto, Toronto, ON, Canada
- Department of Chemistry, University of Waterloo, Waterloo, ON, Canada
| | - E Wolfram
- CEILAP-UNIDEF (MINDEF-CONICET), UMI-IFAECI-CNRS-3351, Villa Martelli, Argentina
| | - J M Zawodny
- NASA Langley Research Center, Hampton, VA, USA
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Douglass AR, Stolarski RS, Strahan SE, Oman LD. Understanding differences in upper stratospheric ozone response to changes in chlorine and temperature as computed using CCMVal-2 models. ACTA ACUST UNITED AC 2012. [DOI: 10.1029/2012jd017483] [Citation(s) in RCA: 16] [Impact Index Per Article: 1.3] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/09/2022]
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Strahan SE, Douglass AR, Stolarski RS, Akiyoshi H, Bekki S, Braesicke P, Butchart N, Chipperfield MP, Cugnet D, Dhomse S, Frith SM, Gettelman A, Hardiman SC, Kinnison DE, Lamarque JF, Mancini E, Marchand M, Michou M, Morgenstern O, Nakamura T, Olivié D, Pawson S, Pitari G, Plummer DA, Pyle JA, Scinocca JF, Shepherd TG, Shibata K, Smale D, Teyssèdre H, Tian W, Yamashita Y. Using transport diagnostics to understand chemistry climate model ozone simulations. ACTA ACUST UNITED AC 2011. [DOI: 10.1029/2010jd015360] [Citation(s) in RCA: 64] [Impact Index Per Article: 4.9] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/09/2022]
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Newman PA, McKenzie R. UV impacts avoided by the Montreal Protocol. Photochem Photobiol Sci 2011; 10:1152-60. [DOI: 10.1039/c0pp00387e] [Citation(s) in RCA: 42] [Impact Index Per Article: 3.2] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/21/2022]
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Austin J, Struthers H, Scinocca J, Plummer DA, Akiyoshi H, Baumgaertner AJG, Bekki S, Bodeker GE, Braesicke P, Brühl C, Butchart N, Chipperfield MP, Cugnet D, Dameris M, Dhomse S, Frith S, Garny H, Gettelman A, Hardiman SC, Jöckel P, Kinnison D, Kubin A, Lamarque JF, Langematz U, Mancini E, Marchand M, Michou M, Morgenstern O, Nakamura T, Nielsen JE, Pitari G, Pyle J, Rozanov E, Shepherd TG, Shibata K, Smale D, Teyssèdre H, Yamashita Y. Chemistry-climate model simulations of spring Antarctic ozone. ACTA ACUST UNITED AC 2010. [DOI: 10.1029/2009jd013577] [Citation(s) in RCA: 49] [Impact Index Per Article: 3.5] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/09/2022]
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10
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Austin J, Scinocca J, Plummer D, Oman L, Waugh D, Akiyoshi H, Bekki S, Braesicke P, Butchart N, Chipperfield M, Cugnet D, Dameris M, Dhomse S, Eyring V, Frith S, Garcia RR, Garny H, Gettelman A, Hardiman SC, Kinnison D, Lamarque JF, Mancini E, Marchand M, Michou M, Morgenstern O, Nakamura T, Pawson S, Pitari G, Pyle J, Rozanov E, Shepherd TG, Shibata K, Teyssèdre H, Wilson RJ, Yamashita Y. Decline and recovery of total column ozone using a multimodel time series analysis. ACTA ACUST UNITED AC 2010. [DOI: 10.1029/2010jd013857] [Citation(s) in RCA: 69] [Impact Index Per Article: 4.9] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/09/2022]
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