The potential of sea ice leads as a predictor for summer Arctic sea ice extent

The Arctic sea ice extent throughout the melt season is closely associated with initial sea ice state in winter and spring. Sea ice leads are important sites of energy fluxes in the Arctic Ocean, which may play an important role in the evolution of Arctic sea ice. In this study, we examine the poten...

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Published in:The Cryosphere
Main Authors: Y. Zhang, X. Cheng, J. Liu, F. Hui
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2018
Subjects:
Online Access:https://doi.org/10.5194/tc-12-3747-2018
https://doaj.org/article/544a1407b43240ae80e96d2f7fb7529b
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spelling ftdoajarticles:oai:doaj.org/article:544a1407b43240ae80e96d2f7fb7529b 2023-05-15T14:32:41+02:00 The potential of sea ice leads as a predictor for summer Arctic sea ice extent Y. Zhang X. Cheng J. Liu F. Hui 2018-11-01T00:00:00Z https://doi.org/10.5194/tc-12-3747-2018 https://doaj.org/article/544a1407b43240ae80e96d2f7fb7529b EN eng Copernicus Publications https://www.the-cryosphere.net/12/3747/2018/tc-12-3747-2018.pdf https://doaj.org/toc/1994-0416 https://doaj.org/toc/1994-0424 doi:10.5194/tc-12-3747-2018 1994-0416 1994-0424 https://doaj.org/article/544a1407b43240ae80e96d2f7fb7529b The Cryosphere, Vol 12, Pp 3747-3757 (2018) Environmental sciences GE1-350 Geology QE1-996.5 article 2018 ftdoajarticles https://doi.org/10.5194/tc-12-3747-2018 2022-12-31T10:42:22Z The Arctic sea ice extent throughout the melt season is closely associated with initial sea ice state in winter and spring. Sea ice leads are important sites of energy fluxes in the Arctic Ocean, which may play an important role in the evolution of Arctic sea ice. In this study, we examine the potential of sea ice leads as a predictor for summer Arctic sea ice extent forecast using a recently developed daily sea ice lead product retrieved from the Moderate-Resolution Imaging Spectroradiometer (MODIS). Our results show that July pan-Arctic sea ice extent can be predicted from the area of sea ice leads integrated from midwinter to late spring, with a prediction error of 0.28 million km 2 that is smaller than the standard deviation of the observed interannual variability. However, the predictive skills for August and September pan-Arctic sea ice extent are very low. When the area of sea ice leads integrated in the Atlantic and central and west Siberian sector of the Arctic is used, it has a significantly strong relationship (high predictability) with both July and August sea ice extent in the Atlantic and central and west Siberian sector of the Arctic. Thus, the realistic representation of sea ice leads (e.g., the areal coverage) in numerical prediction systems might improve the skill of forecast in the Arctic region. Article in Journal/Newspaper Arctic Arctic Ocean Sea ice The Cryosphere Directory of Open Access Journals: DOAJ Articles Arctic Arctic Ocean Midwinter ENVELOPE(139.931,139.931,-66.690,-66.690) The Cryosphere 12 12 3747 3757
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Environmental sciences
GE1-350
Geology
QE1-996.5
spellingShingle Environmental sciences
GE1-350
Geology
QE1-996.5
Y. Zhang
X. Cheng
J. Liu
F. Hui
The potential of sea ice leads as a predictor for summer Arctic sea ice extent
topic_facet Environmental sciences
GE1-350
Geology
QE1-996.5
description The Arctic sea ice extent throughout the melt season is closely associated with initial sea ice state in winter and spring. Sea ice leads are important sites of energy fluxes in the Arctic Ocean, which may play an important role in the evolution of Arctic sea ice. In this study, we examine the potential of sea ice leads as a predictor for summer Arctic sea ice extent forecast using a recently developed daily sea ice lead product retrieved from the Moderate-Resolution Imaging Spectroradiometer (MODIS). Our results show that July pan-Arctic sea ice extent can be predicted from the area of sea ice leads integrated from midwinter to late spring, with a prediction error of 0.28 million km 2 that is smaller than the standard deviation of the observed interannual variability. However, the predictive skills for August and September pan-Arctic sea ice extent are very low. When the area of sea ice leads integrated in the Atlantic and central and west Siberian sector of the Arctic is used, it has a significantly strong relationship (high predictability) with both July and August sea ice extent in the Atlantic and central and west Siberian sector of the Arctic. Thus, the realistic representation of sea ice leads (e.g., the areal coverage) in numerical prediction systems might improve the skill of forecast in the Arctic region.
format Article in Journal/Newspaper
author Y. Zhang
X. Cheng
J. Liu
F. Hui
author_facet Y. Zhang
X. Cheng
J. Liu
F. Hui
author_sort Y. Zhang
title The potential of sea ice leads as a predictor for summer Arctic sea ice extent
title_short The potential of sea ice leads as a predictor for summer Arctic sea ice extent
title_full The potential of sea ice leads as a predictor for summer Arctic sea ice extent
title_fullStr The potential of sea ice leads as a predictor for summer Arctic sea ice extent
title_full_unstemmed The potential of sea ice leads as a predictor for summer Arctic sea ice extent
title_sort potential of sea ice leads as a predictor for summer arctic sea ice extent
publisher Copernicus Publications
publishDate 2018
url https://doi.org/10.5194/tc-12-3747-2018
https://doaj.org/article/544a1407b43240ae80e96d2f7fb7529b
long_lat ENVELOPE(139.931,139.931,-66.690,-66.690)
geographic Arctic
Arctic Ocean
Midwinter
geographic_facet Arctic
Arctic Ocean
Midwinter
genre Arctic
Arctic Ocean
Sea ice
The Cryosphere
genre_facet Arctic
Arctic Ocean
Sea ice
The Cryosphere
op_source The Cryosphere, Vol 12, Pp 3747-3757 (2018)
op_relation https://www.the-cryosphere.net/12/3747/2018/tc-12-3747-2018.pdf
https://doaj.org/toc/1994-0416
https://doaj.org/toc/1994-0424
doi:10.5194/tc-12-3747-2018
1994-0416
1994-0424
https://doaj.org/article/544a1407b43240ae80e96d2f7fb7529b
op_doi https://doi.org/10.5194/tc-12-3747-2018
container_title The Cryosphere
container_volume 12
container_issue 12
container_start_page 3747
op_container_end_page 3757
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