Changing seasonal sea ice predictor relationships in a changing Arctic climate

Seasonal predictions of Arctic sea ice conditions often rely on statistical relationships of a set of predictors that have shown skill for historical conditions. However, with rapid changes occurring in the Arctic climate, it is unclear whether these statistical relationships will remain valid. Here...

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Bibliographic Details
Published in:Geophysical Research Letters
Other Authors: Holland, Marika (author), Stroeve, Julienne (author), American Geophysical Union (sponsor)
Format: Article in Journal/Newspaper
Language:English
Published: 2001
Subjects:
Online Access:http://nldr.library.ucar.edu/repository/collections/OSGC-000-000-010-979
https://doi.org/10.1029/2011GL049303
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spelling ftncar:oai:drupal-site.org:articles_8870 2023-10-01T03:52:41+02:00 Changing seasonal sea ice predictor relationships in a changing Arctic climate Holland, Marika (author) Stroeve, Julienne (author) American Geophysical Union (sponsor) 2001-09-20 application/pdf http://nldr.library.ucar.edu/repository/collections/OSGC-000-000-010-979 https://doi.org/10.1029/2011GL049303 en eng Geophysical Research Letters http://nldr.library.ucar.edu/repository/collections/OSGC-000-000-010-979 doi:10.1029/2011GL049303 ark:/85065/d728089v Copyright 2011 American Geophysical Union. Sea ice Arctic region Ice mechanics Oceanography Mathematical geophysics Prediction Text article 2001 ftncar https://doi.org/10.1029/2011GL049303 2023-09-04T18:26:51Z Seasonal predictions of Arctic sea ice conditions often rely on statistical relationships of a set of predictors that have shown skill for historical conditions. However, with rapid changes occurring in the Arctic climate, it is unclear whether these statistical relationships will remain valid. Here, preindustrial control, present-day control, and 20th-21st century climate model integrations are used to assess predictors for end-of-summer ice extent under various and changing climate conditions. Of importance for future forecasting systems, we find that the variance of September extent anomalies explained by winter-spring sea ice predictors, such as the area of Arctic basin thin ice cover, increases during the transition to a seasonally ice-covered Arctic. In contrast, summer atmospheric circulation variability plays a decreasingly important role in explaining the end-of-summer ice cover anomalies. These changes are primarily related to climate-dependent changes in the location of summer sea ice anomalies. Article in Journal/Newspaper Arctic Basin Arctic Sea ice OpenSky (NCAR/UCAR - National Center for Atmospheric Research/University Corporation for Atmospheric Research) Arctic Geophysical Research Letters 38 18 n/a n/a
institution Open Polar
collection OpenSky (NCAR/UCAR - National Center for Atmospheric Research/University Corporation for Atmospheric Research)
op_collection_id ftncar
language English
topic Sea ice
Arctic region
Ice mechanics
Oceanography
Mathematical geophysics
Prediction
spellingShingle Sea ice
Arctic region
Ice mechanics
Oceanography
Mathematical geophysics
Prediction
Changing seasonal sea ice predictor relationships in a changing Arctic climate
topic_facet Sea ice
Arctic region
Ice mechanics
Oceanography
Mathematical geophysics
Prediction
description Seasonal predictions of Arctic sea ice conditions often rely on statistical relationships of a set of predictors that have shown skill for historical conditions. However, with rapid changes occurring in the Arctic climate, it is unclear whether these statistical relationships will remain valid. Here, preindustrial control, present-day control, and 20th-21st century climate model integrations are used to assess predictors for end-of-summer ice extent under various and changing climate conditions. Of importance for future forecasting systems, we find that the variance of September extent anomalies explained by winter-spring sea ice predictors, such as the area of Arctic basin thin ice cover, increases during the transition to a seasonally ice-covered Arctic. In contrast, summer atmospheric circulation variability plays a decreasingly important role in explaining the end-of-summer ice cover anomalies. These changes are primarily related to climate-dependent changes in the location of summer sea ice anomalies.
author2 Holland, Marika (author)
Stroeve, Julienne (author)
American Geophysical Union (sponsor)
format Article in Journal/Newspaper
title Changing seasonal sea ice predictor relationships in a changing Arctic climate
title_short Changing seasonal sea ice predictor relationships in a changing Arctic climate
title_full Changing seasonal sea ice predictor relationships in a changing Arctic climate
title_fullStr Changing seasonal sea ice predictor relationships in a changing Arctic climate
title_full_unstemmed Changing seasonal sea ice predictor relationships in a changing Arctic climate
title_sort changing seasonal sea ice predictor relationships in a changing arctic climate
publishDate 2001
url http://nldr.library.ucar.edu/repository/collections/OSGC-000-000-010-979
https://doi.org/10.1029/2011GL049303
geographic Arctic
geographic_facet Arctic
genre Arctic Basin
Arctic
Sea ice
genre_facet Arctic Basin
Arctic
Sea ice
op_relation Geophysical Research Letters
http://nldr.library.ucar.edu/repository/collections/OSGC-000-000-010-979
doi:10.1029/2011GL049303
ark:/85065/d728089v
op_rights Copyright 2011 American Geophysical Union.
op_doi https://doi.org/10.1029/2011GL049303
container_title Geophysical Research Letters
container_volume 38
container_issue 18
container_start_page n/a
op_container_end_page n/a
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