Antarctic ozone loss in 1979–2010: first sign of ozone recovery

A long-term ozone loss time series is necessary to understand the evolution of ozone in Antarctica. Therefore, we construct the time series using ground-based, satellite and bias-corrected multi-sensor reanalysis (MSR) data sets for the period 1989–2010. The trends in ozone over 1979–2010 are also e...

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Main Authors: A. Pazmiño, F. Goutail, H. K. Roscoe, J.-P. Pommereau, F. Lefèvre, J. Kuttippurath, J. D. Shanklin
Format: Article
Language:English
Published: Copernicus Publications 2013-02-01
Series:Atmospheric Chemistry and Physics
Online Access:http://www.atmos-chem-phys.net/13/1625/2013/acp-13-1625-2013.pdf
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author A. Pazmiño
F. Goutail
H. K. Roscoe
J.-P. Pommereau
F. Lefèvre
J. Kuttippurath
J. D. Shanklin
author_facet A. Pazmiño
F. Goutail
H. K. Roscoe
J.-P. Pommereau
F. Lefèvre
J. Kuttippurath
J. D. Shanklin
author_sort A. Pazmiño
collection DOAJ
description A long-term ozone loss time series is necessary to understand the evolution of ozone in Antarctica. Therefore, we construct the time series using ground-based, satellite and bias-corrected multi-sensor reanalysis (MSR) data sets for the period 1989–2010. The trends in ozone over 1979–2010 are also estimated to further elucidate its evolution in the wake of decreasing halogen levels in the stratosphere. Our analysis with ground-based observations shows that the average ozone loss in the Antarctic is about −33 to −50% (−90 to −155 DU (Dobson Unit)) in 1989–1992, and then stayed at around −48% (−160 DU). The ozone loss in the warmer winters (e.g. 2002 and 2004) is lower (−37 to −46%), and in the very cold winters (e.g. 2003 and 2006) it is higher (−52 to −55%). These loss estimates are in good agreement with those estimated from satellite observations, where the differences are less than ±3%. The ozone trends based on the equivalent effective Antarctic stratospheric chlorine (EEASC) and piecewise linear trend (PWLT) functions for the vortex averaged ground-based, Total Ozone Mapping Spectrometer/Ozone Monitoring Instrument (TOMS/OMI), and MSR data averaged over September–November exhibit about −4.6 DU yr<sup>−1</sup> over 1979–1999, corroborating the role of halogens in the ozone decrease during the period. The ozone trends computed for the 2000–2010 period are about +1 DU yr<sup>−1</sup> for EEASC and +2.6 DU yr<sup>−1</sup> for the PWLT functions. The larger positive PWLT trends for the 2000–2010 period indicate the influence of dynamics and other basis functions on the increase of ozone. The trends in both periods are significant at 95% confidence intervals for all analyses. Therefore, our study suggests that Antarctic ozone shows a significant positive trend toward its recovery, and hence, leaves a clear signature of the successful implementation of the Montreal Protocol.
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spelling doaj.art-8265763fd3ad4647b68f646d0883eed92022-12-22T00:14:17ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242013-02-011331625163510.5194/acp-13-1625-2013Antarctic ozone loss in 1979&ndash;2010: first sign of ozone recoveryA. PazmiñoF. GoutailH. K. RoscoeJ.-P. PommereauF. LefèvreJ. KuttippurathJ. D. ShanklinA long-term ozone loss time series is necessary to understand the evolution of ozone in Antarctica. Therefore, we construct the time series using ground-based, satellite and bias-corrected multi-sensor reanalysis (MSR) data sets for the period 1989–2010. The trends in ozone over 1979–2010 are also estimated to further elucidate its evolution in the wake of decreasing halogen levels in the stratosphere. Our analysis with ground-based observations shows that the average ozone loss in the Antarctic is about −33 to −50% (−90 to −155 DU (Dobson Unit)) in 1989–1992, and then stayed at around −48% (−160 DU). The ozone loss in the warmer winters (e.g. 2002 and 2004) is lower (−37 to −46%), and in the very cold winters (e.g. 2003 and 2006) it is higher (−52 to −55%). These loss estimates are in good agreement with those estimated from satellite observations, where the differences are less than ±3%. The ozone trends based on the equivalent effective Antarctic stratospheric chlorine (EEASC) and piecewise linear trend (PWLT) functions for the vortex averaged ground-based, Total Ozone Mapping Spectrometer/Ozone Monitoring Instrument (TOMS/OMI), and MSR data averaged over September–November exhibit about −4.6 DU yr<sup>−1</sup> over 1979–1999, corroborating the role of halogens in the ozone decrease during the period. The ozone trends computed for the 2000–2010 period are about +1 DU yr<sup>−1</sup> for EEASC and +2.6 DU yr<sup>−1</sup> for the PWLT functions. The larger positive PWLT trends for the 2000–2010 period indicate the influence of dynamics and other basis functions on the increase of ozone. The trends in both periods are significant at 95% confidence intervals for all analyses. Therefore, our study suggests that Antarctic ozone shows a significant positive trend toward its recovery, and hence, leaves a clear signature of the successful implementation of the Montreal Protocol.http://www.atmos-chem-phys.net/13/1625/2013/acp-13-1625-2013.pdf
spellingShingle A. Pazmiño
F. Goutail
H. K. Roscoe
J.-P. Pommereau
F. Lefèvre
J. Kuttippurath
J. D. Shanklin
Antarctic ozone loss in 1979&ndash;2010: first sign of ozone recovery
Atmospheric Chemistry and Physics
title Antarctic ozone loss in 1979&ndash;2010: first sign of ozone recovery
title_full Antarctic ozone loss in 1979&ndash;2010: first sign of ozone recovery
title_fullStr Antarctic ozone loss in 1979&ndash;2010: first sign of ozone recovery
title_full_unstemmed Antarctic ozone loss in 1979&ndash;2010: first sign of ozone recovery
title_short Antarctic ozone loss in 1979&ndash;2010: first sign of ozone recovery
title_sort antarctic ozone loss in 1979 ndash 2010 first sign of ozone recovery
url http://www.atmos-chem-phys.net/13/1625/2013/acp-13-1625-2013.pdf
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