Prospects for seasonal prediction of summertime trans-Arctic sea ice path

The continuing decline of the summertime sea ice cover has reduced the sea ice path that must be traversed to Arctic destinations and through the Arctic between the Atlantic and Pacific Oceans, stimulating interest in trans-Arctic Ocean routes. Seasonal prediction of the sea ice cover along these ro...

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Published in:Journal of Climate
Other Authors: Winton, Michael (author), Bushuk, Mitchell (author), Zhang, Yongfei (author), Hurlin, Bill (author), Jia, Liwei (author), Johnson, Nathaniel C. (author), Lu, Feiyu (author)
Format: Article in Journal/Newspaper
Language:English
Published: 2022
Subjects:
Online Access:https://doi.org/10.1175/JCLI-D-21-0634.1
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spelling ftncar:oai:drupal-site.org:articles_25940 2023-10-01T03:53:19+02:00 Prospects for seasonal prediction of summertime trans-Arctic sea ice path Winton, Michael (author) Bushuk, Mitchell (author) Zhang, Yongfei (author) Hurlin, Bill (author) Jia, Liwei (author) Johnson, Nathaniel C. (author) Lu, Feiyu (author) 2022-07-01 https://doi.org/10.1175/JCLI-D-21-0634.1 en eng Journal of Climate--0894-8755--1520-0442 Sea Ice Concentrations from Nimbus-7 SMMR and DMSP SSM/I-SSMIS Passive Microwave Data, Version 1--10.5067/8GQ8LZQVL0VL articles:25940 doi:10.1175/JCLI-D-21-0634.1 ark:/85065/d7dn48ww Copyright 2022 American Meteorological Society (AMS). article Text 2022 ftncar https://doi.org/10.1175/JCLI-D-21-0634.1 2023-09-04T18:21:31Z The continuing decline of the summertime sea ice cover has reduced the sea ice path that must be traversed to Arctic destinations and through the Arctic between the Atlantic and Pacific Oceans, stimulating interest in trans-Arctic Ocean routes. Seasonal prediction of the sea ice cover along these routes could support the increasing summertime ship traffic taking advantage of recent low ice conditions. We introduce the minimum Arctic sea ice path (MIP) between Atlantic and Pacific Oceans as a shipping-relevant metric that is amenable to multidecadal hindcast evaluation. We show, using 1992-2017 retrospective predictions, that bias correction is necessary for the GFDL Seamless System for Prediction and Earth System Research (SPEAR) forecast system to improve upon damped persistence seasonal forecasts of summertime daily MIP between the Atlantic and Pacific Oceans both east and west of Greenland, corresponding roughly to the Northeast and Northwest Passages. Without bias correction, only the Northwest Passage MIP forecasts have lower error than a damped persistence forecast. Using the forecast ensemble spread to estimate a lower bound on forecast error, we find large opportunities for forecast error reduction, especially at lead times of less than 2 months. Most of the potential improvement remains after linear removal of climatological and trend biases, suggesting that significant error reduction might come from improved initialization and simulation of subannual variability. Using a different passive microwave sea ice dataset for calculating error than was used for data assimilation increases the raw forecast errors but not the trend anomaly forecast errors. Article in Journal/Newspaper Arctic Arctic Ocean Greenland Northwest passage Sea ice OpenSky (NCAR/UCAR - National Center for Atmospheric Research/University Corporation for Atmospheric Research) Arctic Arctic Ocean Greenland Northwest Passage Pacific Journal of Climate 35 13 4253 4263
institution Open Polar
collection OpenSky (NCAR/UCAR - National Center for Atmospheric Research/University Corporation for Atmospheric Research)
op_collection_id ftncar
language English
description The continuing decline of the summertime sea ice cover has reduced the sea ice path that must be traversed to Arctic destinations and through the Arctic between the Atlantic and Pacific Oceans, stimulating interest in trans-Arctic Ocean routes. Seasonal prediction of the sea ice cover along these routes could support the increasing summertime ship traffic taking advantage of recent low ice conditions. We introduce the minimum Arctic sea ice path (MIP) between Atlantic and Pacific Oceans as a shipping-relevant metric that is amenable to multidecadal hindcast evaluation. We show, using 1992-2017 retrospective predictions, that bias correction is necessary for the GFDL Seamless System for Prediction and Earth System Research (SPEAR) forecast system to improve upon damped persistence seasonal forecasts of summertime daily MIP between the Atlantic and Pacific Oceans both east and west of Greenland, corresponding roughly to the Northeast and Northwest Passages. Without bias correction, only the Northwest Passage MIP forecasts have lower error than a damped persistence forecast. Using the forecast ensemble spread to estimate a lower bound on forecast error, we find large opportunities for forecast error reduction, especially at lead times of less than 2 months. Most of the potential improvement remains after linear removal of climatological and trend biases, suggesting that significant error reduction might come from improved initialization and simulation of subannual variability. Using a different passive microwave sea ice dataset for calculating error than was used for data assimilation increases the raw forecast errors but not the trend anomaly forecast errors.
author2 Winton, Michael (author)
Bushuk, Mitchell (author)
Zhang, Yongfei (author)
Hurlin, Bill (author)
Jia, Liwei (author)
Johnson, Nathaniel C. (author)
Lu, Feiyu (author)
format Article in Journal/Newspaper
title Prospects for seasonal prediction of summertime trans-Arctic sea ice path
spellingShingle Prospects for seasonal prediction of summertime trans-Arctic sea ice path
title_short Prospects for seasonal prediction of summertime trans-Arctic sea ice path
title_full Prospects for seasonal prediction of summertime trans-Arctic sea ice path
title_fullStr Prospects for seasonal prediction of summertime trans-Arctic sea ice path
title_full_unstemmed Prospects for seasonal prediction of summertime trans-Arctic sea ice path
title_sort prospects for seasonal prediction of summertime trans-arctic sea ice path
publishDate 2022
url https://doi.org/10.1175/JCLI-D-21-0634.1
geographic Arctic
Arctic Ocean
Greenland
Northwest Passage
Pacific
geographic_facet Arctic
Arctic Ocean
Greenland
Northwest Passage
Pacific
genre Arctic
Arctic Ocean
Greenland
Northwest passage
Sea ice
genre_facet Arctic
Arctic Ocean
Greenland
Northwest passage
Sea ice
op_relation Journal of Climate--0894-8755--1520-0442
Sea Ice Concentrations from Nimbus-7 SMMR and DMSP SSM/I-SSMIS Passive Microwave Data, Version 1--10.5067/8GQ8LZQVL0VL
articles:25940
doi:10.1175/JCLI-D-21-0634.1
ark:/85065/d7dn48ww
op_rights Copyright 2022 American Meteorological Society (AMS).
op_doi https://doi.org/10.1175/JCLI-D-21-0634.1
container_title Journal of Climate
container_volume 35
container_issue 13
container_start_page 4253
op_container_end_page 4263
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