Observed Antarctic sea ice expansion reproduced in a climate model after correcting biases in sea ice drift velocity

The Antarctic sea ice area expanded significantly during 1979-2015. This is at odds with state-of-the-art climate models, which typically simulate a receding Antarctic sea ice cover in response to increasing greenhouse forcing. Here, we investigate the hypothesis that this discrepancy between models...

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Main Authors: Sun, Shantong, Eisenman, Ian
Format: Article in Journal/Newspaper
Language:unknown
Published: eScholarship, University of California 2021
Subjects:
Online Access:https://escholarship.org/uc/item/6bc7j7j2
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spelling ftcdlib:oai:escholarship.org:ark:/13030/qt6bc7j7j2 2023-11-05T03:35:18+01:00 Observed Antarctic sea ice expansion reproduced in a climate model after correcting biases in sea ice drift velocity Sun, Shantong Eisenman, Ian 1060 2021-01-01 application/pdf https://escholarship.org/uc/item/6bc7j7j2 unknown eScholarship, University of California qt6bc7j7j2 https://escholarship.org/uc/item/6bc7j7j2 public Nature Communications, vol 12, iss 1 Earth Sciences Oceanography Physical Geography and Environmental Geoscience Climate Action article 2021 ftcdlib 2023-10-09T18:05:14Z The Antarctic sea ice area expanded significantly during 1979-2015. This is at odds with state-of-the-art climate models, which typically simulate a receding Antarctic sea ice cover in response to increasing greenhouse forcing. Here, we investigate the hypothesis that this discrepancy between models and observations occurs due to simulation biases in the sea ice drift velocity. As a control we use the Community Earth System Model (CESM) Large Ensemble, which has 40 realizations of past and future climate change that all undergo Antarctic sea ice retreat during recent decades. We modify CESM to replace the simulated sea ice velocity field with a satellite-derived estimate of the observed sea ice motion, and we simulate 3 realizations of recent climate change. We find that the Antarctic sea ice expands in all 3 of these realizations, with the simulated spatial structure of the expansion bearing resemblance to observations. The results suggest that the reason CESM has failed to capture the observed Antarctic sea ice expansion is due to simulation biases in the sea ice drift velocity, implying that an improved representation of sea ice motion is crucial for more accurate sea ice projections. Article in Journal/Newspaper Antarc* Antarctic Sea ice University of California: eScholarship
institution Open Polar
collection University of California: eScholarship
op_collection_id ftcdlib
language unknown
topic Earth Sciences
Oceanography
Physical Geography and Environmental Geoscience
Climate Action
spellingShingle Earth Sciences
Oceanography
Physical Geography and Environmental Geoscience
Climate Action
Sun, Shantong
Eisenman, Ian
Observed Antarctic sea ice expansion reproduced in a climate model after correcting biases in sea ice drift velocity
topic_facet Earth Sciences
Oceanography
Physical Geography and Environmental Geoscience
Climate Action
description The Antarctic sea ice area expanded significantly during 1979-2015. This is at odds with state-of-the-art climate models, which typically simulate a receding Antarctic sea ice cover in response to increasing greenhouse forcing. Here, we investigate the hypothesis that this discrepancy between models and observations occurs due to simulation biases in the sea ice drift velocity. As a control we use the Community Earth System Model (CESM) Large Ensemble, which has 40 realizations of past and future climate change that all undergo Antarctic sea ice retreat during recent decades. We modify CESM to replace the simulated sea ice velocity field with a satellite-derived estimate of the observed sea ice motion, and we simulate 3 realizations of recent climate change. We find that the Antarctic sea ice expands in all 3 of these realizations, with the simulated spatial structure of the expansion bearing resemblance to observations. The results suggest that the reason CESM has failed to capture the observed Antarctic sea ice expansion is due to simulation biases in the sea ice drift velocity, implying that an improved representation of sea ice motion is crucial for more accurate sea ice projections.
format Article in Journal/Newspaper
author Sun, Shantong
Eisenman, Ian
author_facet Sun, Shantong
Eisenman, Ian
author_sort Sun, Shantong
title Observed Antarctic sea ice expansion reproduced in a climate model after correcting biases in sea ice drift velocity
title_short Observed Antarctic sea ice expansion reproduced in a climate model after correcting biases in sea ice drift velocity
title_full Observed Antarctic sea ice expansion reproduced in a climate model after correcting biases in sea ice drift velocity
title_fullStr Observed Antarctic sea ice expansion reproduced in a climate model after correcting biases in sea ice drift velocity
title_full_unstemmed Observed Antarctic sea ice expansion reproduced in a climate model after correcting biases in sea ice drift velocity
title_sort observed antarctic sea ice expansion reproduced in a climate model after correcting biases in sea ice drift velocity
publisher eScholarship, University of California
publishDate 2021
url https://escholarship.org/uc/item/6bc7j7j2
op_coverage 1060
genre Antarc*
Antarctic
Sea ice
genre_facet Antarc*
Antarctic
Sea ice
op_source Nature Communications, vol 12, iss 1
op_relation qt6bc7j7j2
https://escholarship.org/uc/item/6bc7j7j2
op_rights public
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