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Responses of Arctic sea ice to stratospheric ozone depletion

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Responses of Arctic sea ice to stratospheric ozone depletion. / Zhang, Jiankai; Tian, Wenshou; Pyle, John A. et al.
In: Science Bulletin, Vol. 67, No. 11, 15.06.2022, p. 1182-1190.

Research output: Contribution to Journal/Magazine › Journal article › peer-review

Harvard

Zhang, J, Tian, W, Pyle, JA, Keeble, J, Abraham, NL, Chipperfield, MP, Xie, F, Yang, Q, Mu, L, Ren, HL, Wang, L & Xu, M 2022, 'Responses of Arctic sea ice to stratospheric ozone depletion', Science Bulletin, vol. 67, no. 11, pp. 1182-1190. https://doi.org/10.1016/j.scib.2022.03.015

APA

Zhang, J., Tian, W., Pyle, J. A., Keeble, J., Abraham, N. L., Chipperfield, M. P., Xie, F., Yang, Q., Mu, L., Ren, H. L., Wang, L., & Xu, M. (2022). Responses of Arctic sea ice to stratospheric ozone depletion. Science Bulletin, 67(11), 1182-1190. https://doi.org/10.1016/j.scib.2022.03.015

Vancouver

Zhang J, Tian W, Pyle JA, Keeble J, Abraham NL, Chipperfield MP et al. Responses of Arctic sea ice to stratospheric ozone depletion. Science Bulletin. 2022 Jun 15;67(11):1182-1190. Epub 2022 Jun 10. doi: 10.1016/j.scib.2022.03.015

Author

Zhang, Jiankai ; Tian, Wenshou ; Pyle, John A. et al. / Responses of Arctic sea ice to stratospheric ozone depletion. In: Science Bulletin. 2022 ; Vol. 67, No. 11. pp. 1182-1190.

Bibtex

@article{644e16e8d6d147cc8f7816def9eecf74,
title = "Responses of Arctic sea ice to stratospheric ozone depletion",
abstract = "The Arctic has experienced several extreme springtime stratospheric ozone depletion events over the past four decades, particularly in 1997, 2011 and 2020. However, the impact of this stratospheric ozone depletion on the climate system remains poorly understood. Here we show that the stratospheric ozone depletion causes significant reductions in the sea ice concentration (SIC) and the sea ice thickness (SIT) over the Kara Sea, Laptev Sea and East Siberian Sea from spring to summer. This is partially caused by enhanced ice transport from Barents-Kara Sea and East Siberian Sea to the Fram Strait, which is induced by a strengthened and longer lived polar vortex associated with stratospheric ozone depletion. Additionally, cloud longwave radiation and surface albedo feedbacks enhance the melting of Arctic sea ice, particularly along the coast of the Eurasian continent. This study highlights the need for realistic representation of stratosphere-troposphere interactions in order to accurately predict Arctic sea ice loss.",
author = "Jiankai Zhang and Wenshou Tian and Pyle, {John A.} and James Keeble and Abraham, {Nathan Luke} and Chipperfield, {Martyn P.} and Fei Xie and Qinghua Yang and Longjiang Mu and Ren, {Hong Li} and Lin Wang and Mian Xu",
note = "Publisher Copyright: {\textcopyright} 2022 Science China Press",
year = "2022",
month = jun,
day = "15",
doi = "10.1016/j.scib.2022.03.015",
language = "English",
volume = "67",
pages = "1182--1190",
journal = "Science Bulletin",
issn = "2095-9273",
publisher = "Elsevier B.V.",
number = "11",

}

RIS

TY - JOUR

T1 - Responses of Arctic sea ice to stratospheric ozone depletion

AU - Zhang, Jiankai

AU - Tian, Wenshou

AU - Pyle, John A.

AU - Keeble, James

AU - Abraham, Nathan Luke

AU - Chipperfield, Martyn P.

AU - Xie, Fei

AU - Yang, Qinghua

AU - Mu, Longjiang

AU - Ren, Hong Li

AU - Wang, Lin

AU - Xu, Mian

N1 - Publisher Copyright: © 2022 Science China Press

PY - 2022/6/15

Y1 - 2022/6/15

N2 - The Arctic has experienced several extreme springtime stratospheric ozone depletion events over the past four decades, particularly in 1997, 2011 and 2020. However, the impact of this stratospheric ozone depletion on the climate system remains poorly understood. Here we show that the stratospheric ozone depletion causes significant reductions in the sea ice concentration (SIC) and the sea ice thickness (SIT) over the Kara Sea, Laptev Sea and East Siberian Sea from spring to summer. This is partially caused by enhanced ice transport from Barents-Kara Sea and East Siberian Sea to the Fram Strait, which is induced by a strengthened and longer lived polar vortex associated with stratospheric ozone depletion. Additionally, cloud longwave radiation and surface albedo feedbacks enhance the melting of Arctic sea ice, particularly along the coast of the Eurasian continent. This study highlights the need for realistic representation of stratosphere-troposphere interactions in order to accurately predict Arctic sea ice loss.

AB - The Arctic has experienced several extreme springtime stratospheric ozone depletion events over the past four decades, particularly in 1997, 2011 and 2020. However, the impact of this stratospheric ozone depletion on the climate system remains poorly understood. Here we show that the stratospheric ozone depletion causes significant reductions in the sea ice concentration (SIC) and the sea ice thickness (SIT) over the Kara Sea, Laptev Sea and East Siberian Sea from spring to summer. This is partially caused by enhanced ice transport from Barents-Kara Sea and East Siberian Sea to the Fram Strait, which is induced by a strengthened and longer lived polar vortex associated with stratospheric ozone depletion. Additionally, cloud longwave radiation and surface albedo feedbacks enhance the melting of Arctic sea ice, particularly along the coast of the Eurasian continent. This study highlights the need for realistic representation of stratosphere-troposphere interactions in order to accurately predict Arctic sea ice loss.

U2 - 10.1016/j.scib.2022.03.015

DO - 10.1016/j.scib.2022.03.015

M3 - Journal article

AN - SCOPUS:85128119622

VL - 67

SP - 1182

EP - 1190

JO - Science Bulletin

JF - Science Bulletin

SN - 2095-9273

IS - 11

ER -