Detecting recovery of the stratospheric ozone layer

Martyn Chipperfield 1, 2 Slimane Bekki 3 Sandip Dhomse 1 Neil R. P. Harris 4 Birgit Hassler 5 Ryan Hossaini 6 Wolfgang Steinbrecht 7 Rémi Thiéblemont 3 Mark Weber 8
1 SEE - School of Earth and Environment [Leeds]
2 National Centre for Earth Observation
3 SHTI - LATMOS
LATMOS - Laboratoire Atmosphères, Milieux, Observations Spatiales
4 Centre for Atmospheric Informatics and Emissions Technology
5 Bodeker Scientific
6 Lancaster Environment Centre
7 DWD - Deutscher Wetterdienst [Offenbach]
8 IUP - Institute of Environmental Physics [Bremen]
Abstract : As a result of the 1987 Montreal Protocol and its amendments, the atmospheric loading of anthropogenic ozone-depleting substances is decreasing. Accordingly, the stratospheric ozone layer is expected to recover. However, short data records and atmospheric variability confound the search for early signs of recovery, and climate change is masking ozone recovery from ozone-depleting substances in some regions and will increasingly affect the extent of recovery. Here we discuss the nature and timescales of ozone recovery, and explore the extent to which it can be currently detected in different atmospheric regions.
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Article dans une revue
Nature, Nature Publishing Group, 2017, 549 (7671), pp.211 - 218. 〈10.1038/nature23681〉
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https://hal-insu.archives-ouvertes.fr/insu-01649741
Contributeur : Catherine Cardon <>
Soumis le : lundi 27 novembre 2017 - 17:06:29
Dernière modification le : mardi 29 mai 2018 - 12:51:06

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INSU | LATMOS | UPMC | UVSQ | UNIV-PARIS-SACLAY

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Martyn Chipperfield, Slimane Bekki, Sandip Dhomse, Neil R. P. Harris, Birgit Hassler, et al.. Detecting recovery of the stratospheric ozone layer. Nature, Nature Publishing Group, 2017, 549 (7671), pp.211 - 218. 〈10.1038/nature23681〉. 〈insu-01649741〉

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