Less Surface Sea Ice Melt in the CESM2 Improves Arctic Sea Ice Simulation With Minimal Non-Polar Climate Impacts
The authors authors thank the two anonymous reviewers for their constructive and helpful reviews. This study isolates the influence of sea ice mean state on pre-industrial climate and transient 1850–2100 climate change within a fully coupled global model: The Community Earth System Model version 2 (...
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Online Access: | http://hdl.handle.net/1828/14061 https://doi.org/10.1029/2021MS002679 |
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ftuvicpubl:oai:dspace.library.uvic.ca:1828/14061 2023-05-15T13:11:15+02:00 Less Surface Sea Ice Melt in the CESM2 Improves Arctic Sea Ice Simulation With Minimal Non-Polar Climate Impacts Kay, Jennifer E. DeRepentigny, Patricia Holland, Marika M. Bailey, David A. DuVivier, Alice K. Blanchard-Wrigglesworth, Ed Deser, Clara Jahn, Alexandra Singh, Hansi Smith, Madison M. Webster, Melinda A. Edwards, Jim Lee, Sun-Seon Rodgers, Keith B. Rosenbloom, Nan 2022 application/pdf http://hdl.handle.net/1828/14061 https://doi.org/10.1029/2021MS002679 en eng Journal of Advances in Modeling Earth Systems Kay, J. E., DeRepentigny, P., Holland, M. M., Bailey, D. A., DuVivier, A. K., Blanchard-Wrigglesworth, E., et al. (2022). Less surface sea ice melt in the CESM2 improves Arctic sea ice simulation with minimal non-polar climate impacts. Journal of Advances in Modeling Earth Systems, 14(4), e2021MS002679. https://doi.org/10.1029/2021MS002679 https://doi.org/10.1029/2021MS002679 http://hdl.handle.net/1828/14061 ice-free Arctic Ocean sea ice climate surface melt internal variability large initial condition ensemble Article 2022 ftuvicpubl https://doi.org/10.1029/2021MS002679 2022-07-19T23:43:58Z The authors authors thank the two anonymous reviewers for their constructive and helpful reviews. This study isolates the influence of sea ice mean state on pre-industrial climate and transient 1850–2100 climate change within a fully coupled global model: The Community Earth System Model version 2 (CESM2). The CESM2 sea ice model physics is modified to increase surface albedo, reduce surface sea ice melt, and increase Arctic sea ice thickness and late summer cover. Importantly, increased Arctic sea ice in the modified model reduces a present-day late-summer ice cover bias. Of interest to coupled model development, this bias reduction is realized without degrading the global simulation including top-of-atmosphere energy imbalance, surface temperature, surface precipitation, and major modes of climate variability. The influence of these sea ice physics changes on transient 1850–2100 climate change is compared within a large initial condition ensemble framework. Despite similar global warming, the modified model with thicker Arctic sea ice than CESM2 has a delayed and more realistic transition to a seasonally ice free Arctic Ocean. Differences in transient climate change between the modified model and CESM2 are challenging to detect due to large internally generated climate variability. In particular, two common sea ice benchmarks—sea ice sensitivity and sea ice trends—are of limited value for comparing models with similar global warming. More broadly, these results show the importance of a reasonable Arctic sea ice mean state when simulating the transition to an ice-free Arctic Ocean in a warming world. Additionally, this work highlights the importance of large initial condition ensembles for credible model-to-model and observation-model comparisons. J. E. Kay was supported by National Science Foundation (NSF) CAREER 1554659. P. DeRepentigny was supported by the Natural Sciences and Engineering Council of Canada (NSERC), the Fond de recherche du Québec—Nature et Technologies (FRQNT) and the Canadian ... Article in Journal/Newspaper albedo Arctic Arctic Arctic Ocean Climate change Global warming Sea ice University of Victoria (Canada): UVicDSpace Arctic Arctic Ocean Canada Kay ENVELOPE(-60.917,-60.917,-64.117,-64.117) Journal of Advances in Modeling Earth Systems 14 4 |
institution |
Open Polar |
collection |
University of Victoria (Canada): UVicDSpace |
op_collection_id |
ftuvicpubl |
language |
English |
topic |
ice-free Arctic Ocean sea ice climate surface melt internal variability large initial condition ensemble |
spellingShingle |
ice-free Arctic Ocean sea ice climate surface melt internal variability large initial condition ensemble Kay, Jennifer E. DeRepentigny, Patricia Holland, Marika M. Bailey, David A. DuVivier, Alice K. Blanchard-Wrigglesworth, Ed Deser, Clara Jahn, Alexandra Singh, Hansi Smith, Madison M. Webster, Melinda A. Edwards, Jim Lee, Sun-Seon Rodgers, Keith B. Rosenbloom, Nan Less Surface Sea Ice Melt in the CESM2 Improves Arctic Sea Ice Simulation With Minimal Non-Polar Climate Impacts |
topic_facet |
ice-free Arctic Ocean sea ice climate surface melt internal variability large initial condition ensemble |
description |
The authors authors thank the two anonymous reviewers for their constructive and helpful reviews. This study isolates the influence of sea ice mean state on pre-industrial climate and transient 1850–2100 climate change within a fully coupled global model: The Community Earth System Model version 2 (CESM2). The CESM2 sea ice model physics is modified to increase surface albedo, reduce surface sea ice melt, and increase Arctic sea ice thickness and late summer cover. Importantly, increased Arctic sea ice in the modified model reduces a present-day late-summer ice cover bias. Of interest to coupled model development, this bias reduction is realized without degrading the global simulation including top-of-atmosphere energy imbalance, surface temperature, surface precipitation, and major modes of climate variability. The influence of these sea ice physics changes on transient 1850–2100 climate change is compared within a large initial condition ensemble framework. Despite similar global warming, the modified model with thicker Arctic sea ice than CESM2 has a delayed and more realistic transition to a seasonally ice free Arctic Ocean. Differences in transient climate change between the modified model and CESM2 are challenging to detect due to large internally generated climate variability. In particular, two common sea ice benchmarks—sea ice sensitivity and sea ice trends—are of limited value for comparing models with similar global warming. More broadly, these results show the importance of a reasonable Arctic sea ice mean state when simulating the transition to an ice-free Arctic Ocean in a warming world. Additionally, this work highlights the importance of large initial condition ensembles for credible model-to-model and observation-model comparisons. J. E. Kay was supported by National Science Foundation (NSF) CAREER 1554659. P. DeRepentigny was supported by the Natural Sciences and Engineering Council of Canada (NSERC), the Fond de recherche du Québec—Nature et Technologies (FRQNT) and the Canadian ... |
format |
Article in Journal/Newspaper |
author |
Kay, Jennifer E. DeRepentigny, Patricia Holland, Marika M. Bailey, David A. DuVivier, Alice K. Blanchard-Wrigglesworth, Ed Deser, Clara Jahn, Alexandra Singh, Hansi Smith, Madison M. Webster, Melinda A. Edwards, Jim Lee, Sun-Seon Rodgers, Keith B. Rosenbloom, Nan |
author_facet |
Kay, Jennifer E. DeRepentigny, Patricia Holland, Marika M. Bailey, David A. DuVivier, Alice K. Blanchard-Wrigglesworth, Ed Deser, Clara Jahn, Alexandra Singh, Hansi Smith, Madison M. Webster, Melinda A. Edwards, Jim Lee, Sun-Seon Rodgers, Keith B. Rosenbloom, Nan |
author_sort |
Kay, Jennifer E. |
title |
Less Surface Sea Ice Melt in the CESM2 Improves Arctic Sea Ice Simulation With Minimal Non-Polar Climate Impacts |
title_short |
Less Surface Sea Ice Melt in the CESM2 Improves Arctic Sea Ice Simulation With Minimal Non-Polar Climate Impacts |
title_full |
Less Surface Sea Ice Melt in the CESM2 Improves Arctic Sea Ice Simulation With Minimal Non-Polar Climate Impacts |
title_fullStr |
Less Surface Sea Ice Melt in the CESM2 Improves Arctic Sea Ice Simulation With Minimal Non-Polar Climate Impacts |
title_full_unstemmed |
Less Surface Sea Ice Melt in the CESM2 Improves Arctic Sea Ice Simulation With Minimal Non-Polar Climate Impacts |
title_sort |
less surface sea ice melt in the cesm2 improves arctic sea ice simulation with minimal non-polar climate impacts |
publisher |
Journal of Advances in Modeling Earth Systems |
publishDate |
2022 |
url |
http://hdl.handle.net/1828/14061 https://doi.org/10.1029/2021MS002679 |
long_lat |
ENVELOPE(-60.917,-60.917,-64.117,-64.117) |
geographic |
Arctic Arctic Ocean Canada Kay |
geographic_facet |
Arctic Arctic Ocean Canada Kay |
genre |
albedo Arctic Arctic Arctic Ocean Climate change Global warming Sea ice |
genre_facet |
albedo Arctic Arctic Arctic Ocean Climate change Global warming Sea ice |
op_relation |
Kay, J. E., DeRepentigny, P., Holland, M. M., Bailey, D. A., DuVivier, A. K., Blanchard-Wrigglesworth, E., et al. (2022). Less surface sea ice melt in the CESM2 improves Arctic sea ice simulation with minimal non-polar climate impacts. Journal of Advances in Modeling Earth Systems, 14(4), e2021MS002679. https://doi.org/10.1029/2021MS002679 https://doi.org/10.1029/2021MS002679 http://hdl.handle.net/1828/14061 |
op_doi |
https://doi.org/10.1029/2021MS002679 |
container_title |
Journal of Advances in Modeling Earth Systems |
container_volume |
14 |
container_issue |
4 |
_version_ |
1766246525102456832 |