Journal
NATURE
Volume 549, Issue 7671, Pages 211-218Publisher
NATURE PORTFOLIO
DOI: 10.1038/nature23681
Keywords
-
Categories
Funding
- NERC National Centre for Atmospheric Science (NCAS)
- Royal Society Wolfson Merit Award
- Deutsche Forschungsgemeinschaft (DFG) Research Unit SHARP (Stratospheric Change and its Role for Climate Prediction)
- ESA CCI-Ozone project
- LABEX L-IPSL project [ANR-10-LABX-18-01]
- European project StratoClim [603557, FP7-ENV.2013.6.1-2]
- NERC CAST [NE/I030051/1]
- NERC [NE/J02449X/1, nceo020005, NE/N014375/1, NE/G014655/1] Funding Source: UKRI
- Natural Environment Research Council [NE/G014655/1, NE/N014375/1, nceo020005, NE/J02449X/1] Funding Source: researchfish
Ask authors/readers for more resources
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.
Authors
I am an author on this paper
Click your name to claim this paper and add it to your profile.
Reviews
Recommended
No Data Available
Share Paper
