Mulit-year Predictability of Greenland Sea Spring Sea-ice Volume in a Coupled Climate Model

Prediction of sea-ice is not only important for shipping but also for weather as it can have a signicant climatic impact. Therefore sea-ice predictions are important for accurate inter-annual to decadal prediction of climate in coupled climate models. However, to our knowledge there has been little...

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Main Authors: Hermanson, Leon, Sutton, Rowan, Keeley, Sarah
Format: Conference Object
Language:English
Published: 2009
Subjects:
Online Access:https://zenodo.org/record/7355940
https://doi.org/10.5281/zenodo.7355940
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spelling ftzenodo:oai:zenodo.org:7355940 2023-05-15T16:27:46+02:00 Mulit-year Predictability of Greenland Sea Spring Sea-ice Volume in a Coupled Climate Model Hermanson, Leon Sutton, Rowan Keeley, Sarah 2009-11-10 https://zenodo.org/record/7355940 https://doi.org/10.5281/zenodo.7355940 eng eng doi:10.5281/zenodo.7355939 https://zenodo.org/communities/ceda-document-repository https://zenodo.org/record/7355940 https://doi.org/10.5281/zenodo.7355940 oai:zenodo.org:7355940 info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by/4.0/legalcode decadal prediction sea ice Meteorology info:eu-repo/semantics/conferencePoster poster 2009 ftzenodo https://doi.org/10.5281/zenodo.735594010.5281/zenodo.7355939 2023-03-10T14:18:42Z Prediction of sea-ice is not only important for shipping but also for weather as it can have a signicant climatic impact. Therefore sea-ice predictions are important for accurate inter-annual to decadal prediction of climate in coupled climate models. However, to our knowledge there has been little work on how predictable sea-ice is in a coupled atmosphere-ocean-ice model. We have studied the predictability of sea-ice in HadCM3 using case study ensemble experiments with external forcing from the late 20th century designed to emphasize the predictability in the climate system due to initial conditions. Here, we will concentrate on spring (maximum) ice-volume in a box in the Greenland Sea (30W to 10E, 68N to 80N). Model climatology from a control-run shows that this region has high inter-annual variability in sea-ice volume. We find that although ice may almost completely disappear from this area in late autumn, the same anomalies re-appear in the following spring for at least the first four years in three out of four case studies. The mechanism for this appears to be related to persistence of ocean heat content in the initial conditions and the state of the meridional overturning circulation and its associated heat transport. In this model, the atmosphere appears to less important than the ocean in determining the predictability of sea-ice volume in the Greenland Sea. Previously curated at: http://cedadocs.ceda.ac.uk/807/ Event type: other. The publish date on this item was its original completed date. This item was not refereed before the publication Main files in this record: poster-NCAS09-HermansonSuttonKeeley.ppt Item originally deposited with Centre for Environmental Data Analysis (CEDA) document repository by Dr Leon Hermanson. Transferred to CEDA document repository community on Zenodo on 24/11/20 Conference Object Greenland Greenland Sea Sea ice Zenodo Greenland Hermanson ENVELOPE(173.533,173.533,-84.383,-84.383)
institution Open Polar
collection Zenodo
op_collection_id ftzenodo
language English
topic decadal prediction
sea ice
Meteorology
spellingShingle decadal prediction
sea ice
Meteorology
Hermanson, Leon
Sutton, Rowan
Keeley, Sarah
Mulit-year Predictability of Greenland Sea Spring Sea-ice Volume in a Coupled Climate Model
topic_facet decadal prediction
sea ice
Meteorology
description Prediction of sea-ice is not only important for shipping but also for weather as it can have a signicant climatic impact. Therefore sea-ice predictions are important for accurate inter-annual to decadal prediction of climate in coupled climate models. However, to our knowledge there has been little work on how predictable sea-ice is in a coupled atmosphere-ocean-ice model. We have studied the predictability of sea-ice in HadCM3 using case study ensemble experiments with external forcing from the late 20th century designed to emphasize the predictability in the climate system due to initial conditions. Here, we will concentrate on spring (maximum) ice-volume in a box in the Greenland Sea (30W to 10E, 68N to 80N). Model climatology from a control-run shows that this region has high inter-annual variability in sea-ice volume. We find that although ice may almost completely disappear from this area in late autumn, the same anomalies re-appear in the following spring for at least the first four years in three out of four case studies. The mechanism for this appears to be related to persistence of ocean heat content in the initial conditions and the state of the meridional overturning circulation and its associated heat transport. In this model, the atmosphere appears to less important than the ocean in determining the predictability of sea-ice volume in the Greenland Sea. Previously curated at: http://cedadocs.ceda.ac.uk/807/ Event type: other. The publish date on this item was its original completed date. This item was not refereed before the publication Main files in this record: poster-NCAS09-HermansonSuttonKeeley.ppt Item originally deposited with Centre for Environmental Data Analysis (CEDA) document repository by Dr Leon Hermanson. Transferred to CEDA document repository community on Zenodo on 24/11/20
format Conference Object
author Hermanson, Leon
Sutton, Rowan
Keeley, Sarah
author_facet Hermanson, Leon
Sutton, Rowan
Keeley, Sarah
author_sort Hermanson, Leon
title Mulit-year Predictability of Greenland Sea Spring Sea-ice Volume in a Coupled Climate Model
title_short Mulit-year Predictability of Greenland Sea Spring Sea-ice Volume in a Coupled Climate Model
title_full Mulit-year Predictability of Greenland Sea Spring Sea-ice Volume in a Coupled Climate Model
title_fullStr Mulit-year Predictability of Greenland Sea Spring Sea-ice Volume in a Coupled Climate Model
title_full_unstemmed Mulit-year Predictability of Greenland Sea Spring Sea-ice Volume in a Coupled Climate Model
title_sort mulit-year predictability of greenland sea spring sea-ice volume in a coupled climate model
publishDate 2009
url https://zenodo.org/record/7355940
https://doi.org/10.5281/zenodo.7355940
long_lat ENVELOPE(173.533,173.533,-84.383,-84.383)
geographic Greenland
Hermanson
geographic_facet Greenland
Hermanson
genre Greenland
Greenland Sea
Sea ice
genre_facet Greenland
Greenland Sea
Sea ice
op_relation doi:10.5281/zenodo.7355939
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https://zenodo.org/record/7355940
https://doi.org/10.5281/zenodo.7355940
oai:zenodo.org:7355940
op_rights info:eu-repo/semantics/openAccess
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op_doi https://doi.org/10.5281/zenodo.735594010.5281/zenodo.7355939
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