Assessment of Arctic sea ice simulations in CMIP5 models

The Arctic sea ice cover has experienced an unprecedented decline since the late 20th century. As a result, the feedback of sea ice anomalies to atmospheric circulation has been increasingly evidenced. While the climate models almost consistently reproduce the downward trend of sea ice cover, great...

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Main Authors: Wu, Liping, Yang, Xiao-Yi, Hu, Jianyu
Format: Text
Language:English
Published: 2018
Subjects:
Online Access:https://doi.org/10.5194/tc-2018-26
https://tc.copernicus.org/preprints/tc-2018-26/
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spelling ftcopernicus:oai:publications.copernicus.org:tcd66501 2023-05-15T14:50:54+02:00 Assessment of Arctic sea ice simulations in CMIP5 models Wu, Liping Yang, Xiao-Yi Hu, Jianyu 2018-09-26 application/pdf https://doi.org/10.5194/tc-2018-26 https://tc.copernicus.org/preprints/tc-2018-26/ eng eng doi:10.5194/tc-2018-26 https://tc.copernicus.org/preprints/tc-2018-26/ eISSN: 1994-0424 Text 2018 ftcopernicus https://doi.org/10.5194/tc-2018-26 2020-07-20T16:23:22Z The Arctic sea ice cover has experienced an unprecedented decline since the late 20th century. As a result, the feedback of sea ice anomalies to atmospheric circulation has been increasingly evidenced. While the climate models almost consistently reproduce the downward trend of sea ice cover, great dispersion between them still exists. To evaluate the model performance in simulating Arctic sea ice and its potential role in climate change, we constructed a reasonable metric by synthesizing the linear trends and anomalies of the sea ice. We particularly focus on the Barents and Kara seas, where the sea ice anomalies have the greatest potential to feedback the atmosphere. Models can be grouped into three categories according to this criterion. The strong contrast among the multi-model ensemble means in different groups demonstrates the robustness and rationality of this method. The potential factors accounting for the different performance of climate models are further explored. The result shows that the model performance depends more on the ozone datasets prescribed by model rather than on the chemistry representation of ozone. Text Arctic Climate change Sea ice Copernicus Publications: E-Journals Arctic
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description The Arctic sea ice cover has experienced an unprecedented decline since the late 20th century. As a result, the feedback of sea ice anomalies to atmospheric circulation has been increasingly evidenced. While the climate models almost consistently reproduce the downward trend of sea ice cover, great dispersion between them still exists. To evaluate the model performance in simulating Arctic sea ice and its potential role in climate change, we constructed a reasonable metric by synthesizing the linear trends and anomalies of the sea ice. We particularly focus on the Barents and Kara seas, where the sea ice anomalies have the greatest potential to feedback the atmosphere. Models can be grouped into three categories according to this criterion. The strong contrast among the multi-model ensemble means in different groups demonstrates the robustness and rationality of this method. The potential factors accounting for the different performance of climate models are further explored. The result shows that the model performance depends more on the ozone datasets prescribed by model rather than on the chemistry representation of ozone.
format Text
author Wu, Liping
Yang, Xiao-Yi
Hu, Jianyu
spellingShingle Wu, Liping
Yang, Xiao-Yi
Hu, Jianyu
Assessment of Arctic sea ice simulations in CMIP5 models
author_facet Wu, Liping
Yang, Xiao-Yi
Hu, Jianyu
author_sort Wu, Liping
title Assessment of Arctic sea ice simulations in CMIP5 models
title_short Assessment of Arctic sea ice simulations in CMIP5 models
title_full Assessment of Arctic sea ice simulations in CMIP5 models
title_fullStr Assessment of Arctic sea ice simulations in CMIP5 models
title_full_unstemmed Assessment of Arctic sea ice simulations in CMIP5 models
title_sort assessment of arctic sea ice simulations in cmip5 models
publishDate 2018
url https://doi.org/10.5194/tc-2018-26
https://tc.copernicus.org/preprints/tc-2018-26/
geographic Arctic
geographic_facet Arctic
genre Arctic
Climate change
Sea ice
genre_facet Arctic
Climate change
Sea ice
op_source eISSN: 1994-0424
op_relation doi:10.5194/tc-2018-26
https://tc.copernicus.org/preprints/tc-2018-26/
op_doi https://doi.org/10.5194/tc-2018-26
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