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Detecting recovery of the stratospheric ozone layer

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Detecting recovery of the stratospheric ozone layer. / Chipperfield, Martyn P; Bekki, Slimane; Dhomse, Sandip et al.
In: Nature, Vol. 549, No. 7671, 14.09.2017, p. 211-218.

Research output: Contribution to Journal/MagazineJournal articlepeer-review

Harvard

Chipperfield, MP, Bekki, S, Dhomse, S, Harris, NRP, Hassler, B, Hossaini, R, Steinbrecht, W, Thiéblemont, R & Weber, M 2017, 'Detecting recovery of the stratospheric ozone layer', Nature, vol. 549, no. 7671, pp. 211-218. https://doi.org/10.1038/nature23681

APA

Chipperfield, M. P., Bekki, S., Dhomse, S., Harris, N. R. P., Hassler, B., Hossaini, R., Steinbrecht, W., Thiéblemont, R., & Weber, M. (2017). Detecting recovery of the stratospheric ozone layer. Nature, 549(7671), 211-218. https://doi.org/10.1038/nature23681

Vancouver

Chipperfield MP, Bekki S, Dhomse S, Harris NRP, Hassler B, Hossaini R et al. Detecting recovery of the stratospheric ozone layer. Nature. 2017 Sept 14;549(7671):211-218. Epub 2017 Sept 13. doi: 10.1038/nature23681

Author

Chipperfield, Martyn P ; Bekki, Slimane ; Dhomse, Sandip et al. / Detecting recovery of the stratospheric ozone layer. In: Nature. 2017 ; Vol. 549, No. 7671. pp. 211-218.

Bibtex

@article{c3ad88e6c9774987833439221babc65e,
title = "Detecting recovery of the stratospheric ozone layer",
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.",
author = "Chipperfield, {Martyn P} and Slimane Bekki and Sandip Dhomse and Harris, {Neil R P} and Birgit Hassler and Ryan Hossaini and Wolfgang Steinbrecht and R{\'e}mi Thi{\'e}blemont and Mark Weber",
note = "{\textcopyright} 2017 Macmillan Publishers Limited, part of Springer Nature. All rights reserved.",
year = "2017",
month = sep,
day = "14",
doi = "10.1038/nature23681",
language = "English",
volume = "549",
pages = "211--218",
journal = "Nature",
issn = "0028-0836",
publisher = "Nature Publishing Group",
number = "7671",

}

RIS

TY - JOUR

T1 - Detecting recovery of the stratospheric ozone layer

AU - Chipperfield, Martyn P

AU - Bekki, Slimane

AU - Dhomse, Sandip

AU - Harris, Neil R P

AU - Hassler, Birgit

AU - Hossaini, Ryan

AU - Steinbrecht, Wolfgang

AU - Thiéblemont, Rémi

AU - Weber, Mark

N1 - © 2017 Macmillan Publishers Limited, part of Springer Nature. All rights reserved.

PY - 2017/9/14

Y1 - 2017/9/14

N2 - 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.

AB - 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.

U2 - 10.1038/nature23681

DO - 10.1038/nature23681

M3 - Journal article

C2 - 28905899

VL - 549

SP - 211

EP - 218

JO - Nature

JF - Nature

SN - 0028-0836

IS - 7671

ER -