Improved Arctic sea ice thickness projections using bias-corrected CMIP5 simulations

Projections of Arctic sea ice thickness (SIT) have the potential to inform stakeholders about accessibility to the region, but are currently rather uncertain. The latest suite of CMIP5 global climate models (GCMs) produce a wide range of simulated SIT in the historical period (1979–2014) and exhibit...

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Published in:The Cryosphere
Main Authors: N. Melia, K. Haines, E. Hawkins
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2015
Subjects:
geo
Online Access:https://doi.org/10.5194/tc-9-2237-2015
http://www.the-cryosphere.net/9/2237/2015/tc-9-2237-2015.pdf
https://doaj.org/article/317dc9f3d8474ed5810f34787bcdb016
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spelling fttriple:oai:gotriple.eu:oai:doaj.org/article:317dc9f3d8474ed5810f34787bcdb016 2023-05-15T14:42:01+02:00 Improved Arctic sea ice thickness projections using bias-corrected CMIP5 simulations N. Melia K. Haines E. Hawkins 2015-12-01 https://doi.org/10.5194/tc-9-2237-2015 http://www.the-cryosphere.net/9/2237/2015/tc-9-2237-2015.pdf https://doaj.org/article/317dc9f3d8474ed5810f34787bcdb016 en eng Copernicus Publications 1994-0416 1994-0424 doi:10.5194/tc-9-2237-2015 http://www.the-cryosphere.net/9/2237/2015/tc-9-2237-2015.pdf https://doaj.org/article/317dc9f3d8474ed5810f34787bcdb016 undefined The Cryosphere, Vol 9, Iss 6, Pp 2237-2251 (2015) geo envir Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2015 fttriple https://doi.org/10.5194/tc-9-2237-2015 2023-01-22T17:58:05Z Projections of Arctic sea ice thickness (SIT) have the potential to inform stakeholders about accessibility to the region, but are currently rather uncertain. The latest suite of CMIP5 global climate models (GCMs) produce a wide range of simulated SIT in the historical period (1979–2014) and exhibit various biases when compared with the Pan-Arctic Ice–Ocean Modelling and Assimilation System (PIOMAS) sea ice reanalysis. We present a new method to constrain such GCM simulations of SIT via a statistical bias correction technique. The bias correction successfully constrains the spatial SIT distribution and temporal variability in the CMIP5 projections whilst retaining the climatic fluctuations from individual ensemble members. The bias correction acts to reduce the spread in projections of SIT and reveals the significant contributions of climate internal variability in the first half of the century and of scenario uncertainty from the mid-century onwards. The projected date of ice-free conditions in the Arctic under the RCP8.5 high emission scenario occurs in the 2050s, which is a decade earlier than without the bias correction, with potentially significant implications for stakeholders in the Arctic such as the shipping industry. The bias correction methodology developed could be similarly applied to other variables to reduce spread in climate projections more generally. Article in Journal/Newspaper Arctic Sea ice The Cryosphere Unknown Arctic The Cryosphere 9 6 2237 2251
institution Open Polar
collection Unknown
op_collection_id fttriple
language English
topic geo
envir
spellingShingle geo
envir
N. Melia
K. Haines
E. Hawkins
Improved Arctic sea ice thickness projections using bias-corrected CMIP5 simulations
topic_facet geo
envir
description Projections of Arctic sea ice thickness (SIT) have the potential to inform stakeholders about accessibility to the region, but are currently rather uncertain. The latest suite of CMIP5 global climate models (GCMs) produce a wide range of simulated SIT in the historical period (1979–2014) and exhibit various biases when compared with the Pan-Arctic Ice–Ocean Modelling and Assimilation System (PIOMAS) sea ice reanalysis. We present a new method to constrain such GCM simulations of SIT via a statistical bias correction technique. The bias correction successfully constrains the spatial SIT distribution and temporal variability in the CMIP5 projections whilst retaining the climatic fluctuations from individual ensemble members. The bias correction acts to reduce the spread in projections of SIT and reveals the significant contributions of climate internal variability in the first half of the century and of scenario uncertainty from the mid-century onwards. The projected date of ice-free conditions in the Arctic under the RCP8.5 high emission scenario occurs in the 2050s, which is a decade earlier than without the bias correction, with potentially significant implications for stakeholders in the Arctic such as the shipping industry. The bias correction methodology developed could be similarly applied to other variables to reduce spread in climate projections more generally.
format Article in Journal/Newspaper
author N. Melia
K. Haines
E. Hawkins
author_facet N. Melia
K. Haines
E. Hawkins
author_sort N. Melia
title Improved Arctic sea ice thickness projections using bias-corrected CMIP5 simulations
title_short Improved Arctic sea ice thickness projections using bias-corrected CMIP5 simulations
title_full Improved Arctic sea ice thickness projections using bias-corrected CMIP5 simulations
title_fullStr Improved Arctic sea ice thickness projections using bias-corrected CMIP5 simulations
title_full_unstemmed Improved Arctic sea ice thickness projections using bias-corrected CMIP5 simulations
title_sort improved arctic sea ice thickness projections using bias-corrected cmip5 simulations
publisher Copernicus Publications
publishDate 2015
url https://doi.org/10.5194/tc-9-2237-2015
http://www.the-cryosphere.net/9/2237/2015/tc-9-2237-2015.pdf
https://doaj.org/article/317dc9f3d8474ed5810f34787bcdb016
geographic Arctic
geographic_facet Arctic
genre Arctic
Sea ice
The Cryosphere
genre_facet Arctic
Sea ice
The Cryosphere
op_source The Cryosphere, Vol 9, Iss 6, Pp 2237-2251 (2015)
op_relation 1994-0416
1994-0424
doi:10.5194/tc-9-2237-2015
http://www.the-cryosphere.net/9/2237/2015/tc-9-2237-2015.pdf
https://doaj.org/article/317dc9f3d8474ed5810f34787bcdb016
op_rights undefined
op_doi https://doi.org/10.5194/tc-9-2237-2015
container_title The Cryosphere
container_volume 9
container_issue 6
container_start_page 2237
op_container_end_page 2251
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