Evaluating sea ice thickness simulation is critical for projecting a summer ice-free Arctic Ocean

Abstract The rapid decline of Arctic sea ice, including sea ice area (SIA) retreat and sea ice thinning, is a striking manifestation of global climate change. Analysis of 40 CMIP6 models reveals a very large spread in both model simulations of the September SIA and thickness and the timing of a summ...

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Published in:Environmental Research Letters
Main Authors: Zhou, Xiao, Wang, Bin, Huang, Fei
Other Authors: National Natural Science Foundation of China, National Key Scientific Research Program of China, National Science Foundation
Format: Article in Journal/Newspaper
Language:unknown
Published: IOP Publishing 2022
Subjects:
Online Access:http://dx.doi.org/10.1088/1748-9326/ac9d4d
https://iopscience.iop.org/article/10.1088/1748-9326/ac9d4d
https://iopscience.iop.org/article/10.1088/1748-9326/ac9d4d/pdf
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spelling crioppubl:10.1088/1748-9326/ac9d4d 2024-09-15T17:53:27+00:00 Evaluating sea ice thickness simulation is critical for projecting a summer ice-free Arctic Ocean Zhou, Xiao Wang, Bin Huang, Fei National Natural Science Foundation of China National Key Scientific Research Program of China National Science Foundation 2022 http://dx.doi.org/10.1088/1748-9326/ac9d4d https://iopscience.iop.org/article/10.1088/1748-9326/ac9d4d https://iopscience.iop.org/article/10.1088/1748-9326/ac9d4d/pdf unknown IOP Publishing http://creativecommons.org/licenses/by/4.0 https://iopscience.iop.org/info/page/text-and-data-mining Environmental Research Letters volume 17, issue 11, page 114033 ISSN 1748-9326 journal-article 2022 crioppubl https://doi.org/10.1088/1748-9326/ac9d4d 2024-08-26T04:19:30Z Abstract The rapid decline of Arctic sea ice, including sea ice area (SIA) retreat and sea ice thinning, is a striking manifestation of global climate change. Analysis of 40 CMIP6 models reveals a very large spread in both model simulations of the September SIA and thickness and the timing of a summer ice-free Arctic Ocean. The existing SIA-based evaluation metrics are deficient due to observational uncertainty, prominent internal variability, and indirect Arctic response to global forcing. Given the critical roles of sea ice thickness (SIT) in determining Arctic ice variation throughout the seasonal cycle and the April SIT bridging the winter freezing and summer melting processes, we propose two SIT-based metrics, the April mean SIT and summer SIA response to April SIT, to assess climate models’ capability to reproduce the historical change of the Arctic sea ice area. The selected 11 good models reduce the uncertainty in the projected first ice-free Arctic by 70% relative to 11 poor models. The chosen models’ ensemble mean projects the first ice-free year in 2049 (2043) under the shared socio-economic pathways (SSP)2-4.5 (SSP5-8.5) scenario with one standard deviation of the inter-model spread of 12.0 (8.9) years. Article in Journal/Newspaper Arctic Ocean Climate change Sea ice IOP Publishing Environmental Research Letters 17 11 114033
institution Open Polar
collection IOP Publishing
op_collection_id crioppubl
language unknown
description Abstract The rapid decline of Arctic sea ice, including sea ice area (SIA) retreat and sea ice thinning, is a striking manifestation of global climate change. Analysis of 40 CMIP6 models reveals a very large spread in both model simulations of the September SIA and thickness and the timing of a summer ice-free Arctic Ocean. The existing SIA-based evaluation metrics are deficient due to observational uncertainty, prominent internal variability, and indirect Arctic response to global forcing. Given the critical roles of sea ice thickness (SIT) in determining Arctic ice variation throughout the seasonal cycle and the April SIT bridging the winter freezing and summer melting processes, we propose two SIT-based metrics, the April mean SIT and summer SIA response to April SIT, to assess climate models’ capability to reproduce the historical change of the Arctic sea ice area. The selected 11 good models reduce the uncertainty in the projected first ice-free Arctic by 70% relative to 11 poor models. The chosen models’ ensemble mean projects the first ice-free year in 2049 (2043) under the shared socio-economic pathways (SSP)2-4.5 (SSP5-8.5) scenario with one standard deviation of the inter-model spread of 12.0 (8.9) years.
author2 National Natural Science Foundation of China
National Key Scientific Research Program of China
National Science Foundation
format Article in Journal/Newspaper
author Zhou, Xiao
Wang, Bin
Huang, Fei
spellingShingle Zhou, Xiao
Wang, Bin
Huang, Fei
Evaluating sea ice thickness simulation is critical for projecting a summer ice-free Arctic Ocean
author_facet Zhou, Xiao
Wang, Bin
Huang, Fei
author_sort Zhou, Xiao
title Evaluating sea ice thickness simulation is critical for projecting a summer ice-free Arctic Ocean
title_short Evaluating sea ice thickness simulation is critical for projecting a summer ice-free Arctic Ocean
title_full Evaluating sea ice thickness simulation is critical for projecting a summer ice-free Arctic Ocean
title_fullStr Evaluating sea ice thickness simulation is critical for projecting a summer ice-free Arctic Ocean
title_full_unstemmed Evaluating sea ice thickness simulation is critical for projecting a summer ice-free Arctic Ocean
title_sort evaluating sea ice thickness simulation is critical for projecting a summer ice-free arctic ocean
publisher IOP Publishing
publishDate 2022
url http://dx.doi.org/10.1088/1748-9326/ac9d4d
https://iopscience.iop.org/article/10.1088/1748-9326/ac9d4d
https://iopscience.iop.org/article/10.1088/1748-9326/ac9d4d/pdf
genre Arctic Ocean
Climate change
Sea ice
genre_facet Arctic Ocean
Climate change
Sea ice
op_source Environmental Research Letters
volume 17, issue 11, page 114033
ISSN 1748-9326
op_rights http://creativecommons.org/licenses/by/4.0
https://iopscience.iop.org/info/page/text-and-data-mining
op_doi https://doi.org/10.1088/1748-9326/ac9d4d
container_title Environmental Research Letters
container_volume 17
container_issue 11
container_start_page 114033
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