Changing seasonal predictability of Arctic summer sea ice area in a warming climate

We use a large ensemble set of simulations and initialized model forecasts to assess changes in the initial-value seasonal predictability of summer Arctic sea ice area from the late-twentieth to the mid-twenty-first century. Ice thickness is an important seasonal predictor of September ice area beca...

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Published in:Journal of Climate
Other Authors: Holland, Marika M. (author), Landrum, Laura (author), Bailey, David (author), Vavrus, Steve (author)
Format: Article in Journal/Newspaper
Language:English
Published: 2019
Subjects:
Online Access:https://doi.org/10.1175/JCLI-D-19-0034.1
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spelling ftncar:oai:drupal-site.org:articles_22653 2023-09-05T13:17:14+02:00 Changing seasonal predictability of Arctic summer sea ice area in a warming climate Holland, Marika M. (author) Landrum, Laura (author) Bailey, David (author) Vavrus, Steve (author) 2019-08 https://doi.org/10.1175/JCLI-D-19-0034.1 en eng Journal of Climate--J. Climate--0894-8755--1520-0442 Sea Ice Index, Version 3--10.7265/N5K072F8 articles:22653 ark:/85065/d7k93bn9 doi:10.1175/JCLI-D-19-0034.1 Copyright 2019 American Meteorological Society (AMS). article Text 2019 ftncar https://doi.org/10.1175/JCLI-D-19-0034.1 2023-08-14T18:50:18Z We use a large ensemble set of simulations and initialized model forecasts to assess changes in the initial-value seasonal predictability of summer Arctic sea ice area from the late-twentieth to the mid-twenty-first century. Ice thickness is an important seasonal predictor of September ice area because early summer thickness anomalies affect how much melt out occurs. We find that the role of this predictor changes in a warming climate, leading to decadal changes in September ice area predictability. In January-initialized prediction experiments, initialization errors grow over time leading to forecast errors in ice thickness at the beginning of the melt season. The magnitude of this ice thickness forecast error growth for regions important to summer melt out decreases in a warming climate, contributing to enhanced predictability. On the other hand, the influence of early summer thickness anomalies on summer melt out and resulting September ice area increases as the climate warms. Given this, for the same magnitude ice thickness forecast error in early summer, a larger September ice area anomaly results in the warming climate, contributing to reduced predictability. The net result of these competing factors is that a sweet spot for predictability exists when the ice thickness forecast error growth is modest and the influence of these errors on melt out is modest. This occurs at about 2010 in our simulations. The predictability of summer ice area is lower for earlier decades, because of higher ice thickness forecast error growth, and for later decades because of a stronger influence of ice thickness forecast errors on summer melt out. NA15OAR4310167 1852977 Article in Journal/Newspaper Arctic Sea ice OpenSky (NCAR/UCAR - National Center for Atmospheric Research/University Corporation for Atmospheric Research) Arctic Journal of Climate 32 16 4963 4979
institution Open Polar
collection OpenSky (NCAR/UCAR - National Center for Atmospheric Research/University Corporation for Atmospheric Research)
op_collection_id ftncar
language English
description We use a large ensemble set of simulations and initialized model forecasts to assess changes in the initial-value seasonal predictability of summer Arctic sea ice area from the late-twentieth to the mid-twenty-first century. Ice thickness is an important seasonal predictor of September ice area because early summer thickness anomalies affect how much melt out occurs. We find that the role of this predictor changes in a warming climate, leading to decadal changes in September ice area predictability. In January-initialized prediction experiments, initialization errors grow over time leading to forecast errors in ice thickness at the beginning of the melt season. The magnitude of this ice thickness forecast error growth for regions important to summer melt out decreases in a warming climate, contributing to enhanced predictability. On the other hand, the influence of early summer thickness anomalies on summer melt out and resulting September ice area increases as the climate warms. Given this, for the same magnitude ice thickness forecast error in early summer, a larger September ice area anomaly results in the warming climate, contributing to reduced predictability. The net result of these competing factors is that a sweet spot for predictability exists when the ice thickness forecast error growth is modest and the influence of these errors on melt out is modest. This occurs at about 2010 in our simulations. The predictability of summer ice area is lower for earlier decades, because of higher ice thickness forecast error growth, and for later decades because of a stronger influence of ice thickness forecast errors on summer melt out. NA15OAR4310167 1852977
author2 Holland, Marika M. (author)
Landrum, Laura (author)
Bailey, David (author)
Vavrus, Steve (author)
format Article in Journal/Newspaper
title Changing seasonal predictability of Arctic summer sea ice area in a warming climate
spellingShingle Changing seasonal predictability of Arctic summer sea ice area in a warming climate
title_short Changing seasonal predictability of Arctic summer sea ice area in a warming climate
title_full Changing seasonal predictability of Arctic summer sea ice area in a warming climate
title_fullStr Changing seasonal predictability of Arctic summer sea ice area in a warming climate
title_full_unstemmed Changing seasonal predictability of Arctic summer sea ice area in a warming climate
title_sort changing seasonal predictability of arctic summer sea ice area in a warming climate
publishDate 2019
url https://doi.org/10.1175/JCLI-D-19-0034.1
geographic Arctic
geographic_facet Arctic
genre Arctic
Sea ice
genre_facet Arctic
Sea ice
op_relation Journal of Climate--J. Climate--0894-8755--1520-0442
Sea Ice Index, Version 3--10.7265/N5K072F8
articles:22653
ark:/85065/d7k93bn9
doi:10.1175/JCLI-D-19-0034.1
op_rights Copyright 2019 American Meteorological Society (AMS).
op_doi https://doi.org/10.1175/JCLI-D-19-0034.1
container_title Journal of Climate
container_volume 32
container_issue 16
container_start_page 4963
op_container_end_page 4979
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