Consistent biases in Antarctic sea ice concentration simulated by climate models

The simulation of Antarctic sea ice in global climate models often does not agree with observations. In this study, we examine the compactness of sea ice, as well as the regional distribution of sea ice concentration, in climate models from the latest Coupled Model Intercomparison Project (CMIP5) an...

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Published in:The Cryosphere
Main Authors: L. A. Roach, S. M. Dean, J. A. Renwick
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2018
Subjects:
geo
Online Access:https://doi.org/10.5194/tc-12-365-2018
https://www.the-cryosphere.net/12/365/2018/tc-12-365-2018.pdf
https://doaj.org/article/68f0b52805a045d398506e5bbebd1cbc
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spelling fttriple:oai:gotriple.eu:oai:doaj.org/article:68f0b52805a045d398506e5bbebd1cbc 2023-05-15T13:43:15+02:00 Consistent biases in Antarctic sea ice concentration simulated by climate models L. A. Roach S. M. Dean J. A. Renwick 2018-01-01 https://doi.org/10.5194/tc-12-365-2018 https://www.the-cryosphere.net/12/365/2018/tc-12-365-2018.pdf https://doaj.org/article/68f0b52805a045d398506e5bbebd1cbc en eng Copernicus Publications doi:10.5194/tc-12-365-2018 1994-0416 1994-0424 https://www.the-cryosphere.net/12/365/2018/tc-12-365-2018.pdf https://doaj.org/article/68f0b52805a045d398506e5bbebd1cbc undefined The Cryosphere, Vol 12, Pp 365-383 (2018) geo envir Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2018 fttriple https://doi.org/10.5194/tc-12-365-2018 2023-01-22T19:11:42Z The simulation of Antarctic sea ice in global climate models often does not agree with observations. In this study, we examine the compactness of sea ice, as well as the regional distribution of sea ice concentration, in climate models from the latest Coupled Model Intercomparison Project (CMIP5) and in satellite observations. We find substantial differences in concentration values between different sets of satellite observations, particularly at high concentrations, requiring careful treatment when comparing to models. As a fraction of total sea ice extent, models simulate too much loose, low-concentration sea ice cover throughout the year, and too little compact, high-concentration cover in the summer. In spite of the differences in physics between models, these tendencies are broadly consistent across the population of 40 CMIP5 simulations, a result not previously highlighted. Separating models with and without an explicit lateral melt term, we find that inclusion of lateral melt may account for overestimation of low-concentration cover. Targeted model experiments with a coupled ocean–sea ice model show that choice of constant floe diameter in the lateral melt scheme can also impact representation of loose ice. This suggests that current sea ice thermodynamics contribute to the inadequate simulation of the low-concentration regime in many models. Article in Journal/Newspaper Antarc* Antarctic Sea ice The Cryosphere Unknown Antarctic The Cryosphere 12 1 365 383
institution Open Polar
collection Unknown
op_collection_id fttriple
language English
topic geo
envir
spellingShingle geo
envir
L. A. Roach
S. M. Dean
J. A. Renwick
Consistent biases in Antarctic sea ice concentration simulated by climate models
topic_facet geo
envir
description The simulation of Antarctic sea ice in global climate models often does not agree with observations. In this study, we examine the compactness of sea ice, as well as the regional distribution of sea ice concentration, in climate models from the latest Coupled Model Intercomparison Project (CMIP5) and in satellite observations. We find substantial differences in concentration values between different sets of satellite observations, particularly at high concentrations, requiring careful treatment when comparing to models. As a fraction of total sea ice extent, models simulate too much loose, low-concentration sea ice cover throughout the year, and too little compact, high-concentration cover in the summer. In spite of the differences in physics between models, these tendencies are broadly consistent across the population of 40 CMIP5 simulations, a result not previously highlighted. Separating models with and without an explicit lateral melt term, we find that inclusion of lateral melt may account for overestimation of low-concentration cover. Targeted model experiments with a coupled ocean–sea ice model show that choice of constant floe diameter in the lateral melt scheme can also impact representation of loose ice. This suggests that current sea ice thermodynamics contribute to the inadequate simulation of the low-concentration regime in many models.
format Article in Journal/Newspaper
author L. A. Roach
S. M. Dean
J. A. Renwick
author_facet L. A. Roach
S. M. Dean
J. A. Renwick
author_sort L. A. Roach
title Consistent biases in Antarctic sea ice concentration simulated by climate models
title_short Consistent biases in Antarctic sea ice concentration simulated by climate models
title_full Consistent biases in Antarctic sea ice concentration simulated by climate models
title_fullStr Consistent biases in Antarctic sea ice concentration simulated by climate models
title_full_unstemmed Consistent biases in Antarctic sea ice concentration simulated by climate models
title_sort consistent biases in antarctic sea ice concentration simulated by climate models
publisher Copernicus Publications
publishDate 2018
url https://doi.org/10.5194/tc-12-365-2018
https://www.the-cryosphere.net/12/365/2018/tc-12-365-2018.pdf
https://doaj.org/article/68f0b52805a045d398506e5bbebd1cbc
geographic Antarctic
geographic_facet Antarctic
genre Antarc*
Antarctic
Sea ice
The Cryosphere
genre_facet Antarc*
Antarctic
Sea ice
The Cryosphere
op_source The Cryosphere, Vol 12, Pp 365-383 (2018)
op_relation doi:10.5194/tc-12-365-2018
1994-0416
1994-0424
https://www.the-cryosphere.net/12/365/2018/tc-12-365-2018.pdf
https://doaj.org/article/68f0b52805a045d398506e5bbebd1cbc
op_rights undefined
op_doi https://doi.org/10.5194/tc-12-365-2018
container_title The Cryosphere
container_volume 12
container_issue 1
container_start_page 365
op_container_end_page 383
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