A Comparison of Arctic Ocean Sea Ice Export Between Nares Strait and the Canadian Arctic Archipelago
Nares Strait and the channels of the Canadian Arctic Archipelago (CAA) act as conduits for sea ice export from the Arctic Ocean but have never been directly compared. Here, we perform such a comparison for both the sea ice area and volume fluxes from October 2016 to December 2021. Nares Strait provi...
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Veröffentlicht in: | Journal of geophysical research. Oceans 2023-04, Vol.128 (4), p.n/a |
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description | Nares Strait and the channels of the Canadian Arctic Archipelago (CAA) act as conduits for sea ice export from the Arctic Ocean but have never been directly compared. Here, we perform such a comparison for both the sea ice area and volume fluxes from October 2016 to December 2021. Nares Strait provided the largest average seasonal (October through September) ice area flux of 95 ± 8 × 103 km2 followed by the CAA regions of the Queen Elizabeth Islands (QEI) at 41 ± 7 × 103 km2 and M’Clure Strait at 2 ± 8 × 103 km2 with corresponding ice volume fluxes of 177 ± 15 km3, 59 ± 10 km3, and 8 ± 8 km3, respectively. Larger Arctic Ocean ice export at Nares Strait was associated with a shorter ice arch duration (237 days) compared to M’Clure Strait (163 days) and QEI (65 days). Seasonal Arctic Ocean ice export was dominated by Nares Strait in 2017–2019 and 2021 but was remarkably exceeded by the QEI in 2020. Large‐scale atmospheric circulation patterns were found to influence the ice area flux in the absence of ice arches but no occurrence of coherent Arctic Ocean ice export events coinciding across all gates were observed. Average net seasonal Arctic Ocean ice area and volume export were 138 × 103 km2 and 245 km3, which represent ∼16% of the area and ∼25% of the volume of sea ice export from Fram Strait. Divergent Arctic Ocean export ice trajectories are apparent for Nares Strait and the QEI when compared to Fram Strait.
Plain Language Summary
Sea ice is transported out of the Arctic Ocean via Nares Strait and the channels of the Canadian Arctic Archipelago (CAA) but these export passageways have never been directly compared. Here, we perform such a comparison for both the sea ice area and volume fluxes from October 2016 to December 2021. Nares Strait provided the largest average seasonal fluxes followed by the CAA regions of the Queen Elizabeth Islands (QEI) and M’Clure Strait. Larger Arctic Ocean ice export at Nares Strait was associated less frequent ice arch formation that halts ice export compared to M’Clure Strait and QEI. No occurrence of a large Arctic Ocean ice export event coinciding across all regions was observed. Arctic Ocean ice export was dominated by Nares Strait in 2017–2019 and 2021 but was remarkably exceeded by the QEI in 2020. Under continued warming, Arctic Ocean ice export from Nares Strait and the QEI are expected to increase.
Key Points
First comparison of Arctic Ocean ice export between Nares Strait and the CAA
No occurrence of large Arctic |
doi_str_mv | 10.1029/2023JC019687 |
format | Article |
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Plain Language Summary
Sea ice is transported out of the Arctic Ocean via Nares Strait and the channels of the Canadian Arctic Archipelago (CAA) but these export passageways have never been directly compared. Here, we perform such a comparison for both the sea ice area and volume fluxes from October 2016 to December 2021. Nares Strait provided the largest average seasonal fluxes followed by the CAA regions of the Queen Elizabeth Islands (QEI) and M’Clure Strait. Larger Arctic Ocean ice export at Nares Strait was associated less frequent ice arch formation that halts ice export compared to M’Clure Strait and QEI. No occurrence of a large Arctic Ocean ice export event coinciding across all regions was observed. Arctic Ocean ice export was dominated by Nares Strait in 2017–2019 and 2021 but was remarkably exceeded by the QEI in 2020. Under continued warming, Arctic Ocean ice export from Nares Strait and the QEI are expected to increase.
Key Points
First comparison of Arctic Ocean ice export between Nares Strait and the CAA
No occurrence of large Arctic Ocean ice export events coinciding across all regions was observed
Seasonal Arctic Ocean ice volume export from Nares Strait and the CAA together represent ∼25% of the volume export from Fram Strait</description><identifier>ISSN: 2169-9275</identifier><identifier>ISSN: 2169-9291</identifier><identifier>EISSN: 2169-9291</identifier><identifier>DOI: 10.1029/2023JC019687</identifier><language>eng</language><publisher>Washington: Blackwell Publishing Ltd</publisher><subject>Arches ; Archipelagoes ; Arctic sea ice ; area flux ; Atmospheric circulation ; Atmospheric circulation patterns ; CAA ; Channels ; dynamics ; Fluxes ; Geophysics ; Ice formation ; Ice volume ; Islands ; Nares Strait ; Ocean warming ; Oceans ; Passageways ; Sea ice ; Straits ; Temperature ; volume flux</subject><ispartof>Journal of geophysical research. Oceans, 2023-04, Vol.128 (4), p.n/a</ispartof><rights>2023 His Majesty the King in Right of Canada and The Authors. Reproduced with the permission of the Minister of Environment and Climate Change.</rights><rights>2023. This article is published under http://creativecommons.org/licenses/by-nc-nd/4.0/ (the “License”). Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License.</rights><rights>info:eu-repo/semantics/openAccess</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a3927-e5dd6f54ca70ee8378e19bff15c802d4c0d9cd5e890fd77e63a8ff4fbb44a4d63</citedby><cites>FETCH-LOGICAL-a3927-e5dd6f54ca70ee8378e19bff15c802d4c0d9cd5e890fd77e63a8ff4fbb44a4d63</cites><orcidid>0000-0002-7372-1007 ; 0000-0002-3986-5605 ; 0000-0002-7427-8094 ; 0000-0001-8263-0951 ; 0000-0002-4848-9867</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://onlinelibrary.wiley.com/doi/pdf/10.1029%2F2023JC019687$$EPDF$$P50$$Gwiley$$Hfree_for_read</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1029%2F2023JC019687$$EHTML$$P50$$Gwiley$$Hfree_for_read</linktohtml><link.rule.ids>230,314,780,784,885,1417,26567,27924,27925,45574,45575</link.rule.ids></links><search><creatorcontrib>Howell, S. E. L.</creatorcontrib><creatorcontrib>Babb, D. G.</creatorcontrib><creatorcontrib>Landy, J. C.</creatorcontrib><creatorcontrib>Moore, G. W. K.</creatorcontrib><creatorcontrib>Montpetit, B.</creatorcontrib><creatorcontrib>Brady, M.</creatorcontrib><title>A Comparison of Arctic Ocean Sea Ice Export Between Nares Strait and the Canadian Arctic Archipelago</title><title>Journal of geophysical research. Oceans</title><description>Nares Strait and the channels of the Canadian Arctic Archipelago (CAA) act as conduits for sea ice export from the Arctic Ocean but have never been directly compared. Here, we perform such a comparison for both the sea ice area and volume fluxes from October 2016 to December 2021. Nares Strait provided the largest average seasonal (October through September) ice area flux of 95 ± 8 × 103 km2 followed by the CAA regions of the Queen Elizabeth Islands (QEI) at 41 ± 7 × 103 km2 and M’Clure Strait at 2 ± 8 × 103 km2 with corresponding ice volume fluxes of 177 ± 15 km3, 59 ± 10 km3, and 8 ± 8 km3, respectively. Larger Arctic Ocean ice export at Nares Strait was associated with a shorter ice arch duration (237 days) compared to M’Clure Strait (163 days) and QEI (65 days). Seasonal Arctic Ocean ice export was dominated by Nares Strait in 2017–2019 and 2021 but was remarkably exceeded by the QEI in 2020. Large‐scale atmospheric circulation patterns were found to influence the ice area flux in the absence of ice arches but no occurrence of coherent Arctic Ocean ice export events coinciding across all gates were observed. Average net seasonal Arctic Ocean ice area and volume export were 138 × 103 km2 and 245 km3, which represent ∼16% of the area and ∼25% of the volume of sea ice export from Fram Strait. Divergent Arctic Ocean export ice trajectories are apparent for Nares Strait and the QEI when compared to Fram Strait.
Plain Language Summary
Sea ice is transported out of the Arctic Ocean via Nares Strait and the channels of the Canadian Arctic Archipelago (CAA) but these export passageways have never been directly compared. Here, we perform such a comparison for both the sea ice area and volume fluxes from October 2016 to December 2021. Nares Strait provided the largest average seasonal fluxes followed by the CAA regions of the Queen Elizabeth Islands (QEI) and M’Clure Strait. Larger Arctic Ocean ice export at Nares Strait was associated less frequent ice arch formation that halts ice export compared to M’Clure Strait and QEI. No occurrence of a large Arctic Ocean ice export event coinciding across all regions was observed. Arctic Ocean ice export was dominated by Nares Strait in 2017–2019 and 2021 but was remarkably exceeded by the QEI in 2020. Under continued warming, Arctic Ocean ice export from Nares Strait and the QEI are expected to increase.
Key Points
First comparison of Arctic Ocean ice export between Nares Strait and the CAA
No occurrence of large Arctic Ocean ice export events coinciding across all regions was observed
Seasonal Arctic Ocean ice volume export from Nares Strait and the CAA together represent ∼25% of the volume export from Fram Strait</description><subject>Arches</subject><subject>Archipelagoes</subject><subject>Arctic sea ice</subject><subject>area flux</subject><subject>Atmospheric circulation</subject><subject>Atmospheric circulation patterns</subject><subject>CAA</subject><subject>Channels</subject><subject>dynamics</subject><subject>Fluxes</subject><subject>Geophysics</subject><subject>Ice formation</subject><subject>Ice volume</subject><subject>Islands</subject><subject>Nares Strait</subject><subject>Ocean warming</subject><subject>Oceans</subject><subject>Passageways</subject><subject>Sea ice</subject><subject>Straits</subject><subject>Temperature</subject><subject>volume flux</subject><issn>2169-9275</issn><issn>2169-9291</issn><issn>2169-9291</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2023</creationdate><recordtype>article</recordtype><sourceid>24P</sourceid><sourceid>WIN</sourceid><sourceid>3HK</sourceid><recordid>eNp9kM1LAzEQxRdRULQ37wa8upqv3STHumitFAt-nEOaTGykbtbsSu1_b6QqnpzLm8NvHm9eURwTfE4wVRcUU3bbYKJqKXaKA0pqVSqqyO7vLqr9YtT3LziPJJJzdVC4MWria2dS6GOLokfjZIdg0dyCadEDGDS1gK4-upgGdAnDGqBFdyZBjx6GZMKATOvQsATUmNa4kI--HbIsQwcr8xyPij1vVj2MvvWweLq-emxuytl8Mm3Gs9KwnK6EyrnaV9wagQEkExKIWnhPKisxddxip6yrQCrsnRBQMyO9536x4NxwV7PD4mTra_M7Q2h1G5PRBGMmNMM1EZk43RJdim_v0A_6Jb6nNofSVOIaC1VTmamzH5_Y9wm87lJ4NWmTvfRX2fpv2RlnW3wdVrD5l9W3k_uGVrwS7BN6xX33</recordid><startdate>202304</startdate><enddate>202304</enddate><creator>Howell, S. E. L.</creator><creator>Babb, D. G.</creator><creator>Landy, J. C.</creator><creator>Moore, G. W. K.</creator><creator>Montpetit, B.</creator><creator>Brady, M.</creator><general>Blackwell Publishing Ltd</general><general>American Chemical Society</general><scope>24P</scope><scope>WIN</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7TG</scope><scope>7TN</scope><scope>F1W</scope><scope>H96</scope><scope>KL.</scope><scope>L.G</scope><scope>3HK</scope><orcidid>https://orcid.org/0000-0002-7372-1007</orcidid><orcidid>https://orcid.org/0000-0002-3986-5605</orcidid><orcidid>https://orcid.org/0000-0002-7427-8094</orcidid><orcidid>https://orcid.org/0000-0001-8263-0951</orcidid><orcidid>https://orcid.org/0000-0002-4848-9867</orcidid></search><sort><creationdate>202304</creationdate><title>A Comparison of Arctic Ocean Sea Ice Export Between Nares Strait and the Canadian Arctic Archipelago</title><author>Howell, S. E. L. ; Babb, D. G. ; Landy, J. C. ; Moore, G. W. K. ; Montpetit, B. ; Brady, M.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a3927-e5dd6f54ca70ee8378e19bff15c802d4c0d9cd5e890fd77e63a8ff4fbb44a4d63</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2023</creationdate><topic>Arches</topic><topic>Archipelagoes</topic><topic>Arctic sea ice</topic><topic>area flux</topic><topic>Atmospheric circulation</topic><topic>Atmospheric circulation patterns</topic><topic>CAA</topic><topic>Channels</topic><topic>dynamics</topic><topic>Fluxes</topic><topic>Geophysics</topic><topic>Ice formation</topic><topic>Ice volume</topic><topic>Islands</topic><topic>Nares Strait</topic><topic>Ocean warming</topic><topic>Oceans</topic><topic>Passageways</topic><topic>Sea ice</topic><topic>Straits</topic><topic>Temperature</topic><topic>volume flux</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Howell, S. E. L.</creatorcontrib><creatorcontrib>Babb, D. G.</creatorcontrib><creatorcontrib>Landy, J. C.</creatorcontrib><creatorcontrib>Moore, G. W. K.</creatorcontrib><creatorcontrib>Montpetit, B.</creatorcontrib><creatorcontrib>Brady, M.</creatorcontrib><collection>Wiley Online Library (Open Access Collection)</collection><collection>Wiley Online Library Free Content</collection><collection>CrossRef</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Oceanic Abstracts</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>NORA - Norwegian Open Research Archives</collection><jtitle>Journal of geophysical research. Oceans</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Howell, S. E. L.</au><au>Babb, D. G.</au><au>Landy, J. C.</au><au>Moore, G. W. K.</au><au>Montpetit, B.</au><au>Brady, M.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>A Comparison of Arctic Ocean Sea Ice Export Between Nares Strait and the Canadian Arctic Archipelago</atitle><jtitle>Journal of geophysical research. Oceans</jtitle><date>2023-04</date><risdate>2023</risdate><volume>128</volume><issue>4</issue><epage>n/a</epage><issn>2169-9275</issn><issn>2169-9291</issn><eissn>2169-9291</eissn><abstract>Nares Strait and the channels of the Canadian Arctic Archipelago (CAA) act as conduits for sea ice export from the Arctic Ocean but have never been directly compared. Here, we perform such a comparison for both the sea ice area and volume fluxes from October 2016 to December 2021. Nares Strait provided the largest average seasonal (October through September) ice area flux of 95 ± 8 × 103 km2 followed by the CAA regions of the Queen Elizabeth Islands (QEI) at 41 ± 7 × 103 km2 and M’Clure Strait at 2 ± 8 × 103 km2 with corresponding ice volume fluxes of 177 ± 15 km3, 59 ± 10 km3, and 8 ± 8 km3, respectively. Larger Arctic Ocean ice export at Nares Strait was associated with a shorter ice arch duration (237 days) compared to M’Clure Strait (163 days) and QEI (65 days). Seasonal Arctic Ocean ice export was dominated by Nares Strait in 2017–2019 and 2021 but was remarkably exceeded by the QEI in 2020. Large‐scale atmospheric circulation patterns were found to influence the ice area flux in the absence of ice arches but no occurrence of coherent Arctic Ocean ice export events coinciding across all gates were observed. Average net seasonal Arctic Ocean ice area and volume export were 138 × 103 km2 and 245 km3, which represent ∼16% of the area and ∼25% of the volume of sea ice export from Fram Strait. Divergent Arctic Ocean export ice trajectories are apparent for Nares Strait and the QEI when compared to Fram Strait.
Plain Language Summary
Sea ice is transported out of the Arctic Ocean via Nares Strait and the channels of the Canadian Arctic Archipelago (CAA) but these export passageways have never been directly compared. Here, we perform such a comparison for both the sea ice area and volume fluxes from October 2016 to December 2021. Nares Strait provided the largest average seasonal fluxes followed by the CAA regions of the Queen Elizabeth Islands (QEI) and M’Clure Strait. Larger Arctic Ocean ice export at Nares Strait was associated less frequent ice arch formation that halts ice export compared to M’Clure Strait and QEI. No occurrence of a large Arctic Ocean ice export event coinciding across all regions was observed. Arctic Ocean ice export was dominated by Nares Strait in 2017–2019 and 2021 but was remarkably exceeded by the QEI in 2020. Under continued warming, Arctic Ocean ice export from Nares Strait and the QEI are expected to increase.
Key Points
First comparison of Arctic Ocean ice export between Nares Strait and the CAA
No occurrence of large Arctic Ocean ice export events coinciding across all regions was observed
Seasonal Arctic Ocean ice volume export from Nares Strait and the CAA together represent ∼25% of the volume export from Fram Strait</abstract><cop>Washington</cop><pub>Blackwell Publishing Ltd</pub><doi>10.1029/2023JC019687</doi><tpages>15</tpages><orcidid>https://orcid.org/0000-0002-7372-1007</orcidid><orcidid>https://orcid.org/0000-0002-3986-5605</orcidid><orcidid>https://orcid.org/0000-0002-7427-8094</orcidid><orcidid>https://orcid.org/0000-0001-8263-0951</orcidid><orcidid>https://orcid.org/0000-0002-4848-9867</orcidid><oa>free_for_read</oa></addata></record> |
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subjects | Arches Archipelagoes Arctic sea ice area flux Atmospheric circulation Atmospheric circulation patterns CAA Channels dynamics Fluxes Geophysics Ice formation Ice volume Islands Nares Strait Ocean warming Oceans Passageways Sea ice Straits Temperature volume flux |
title | A Comparison of Arctic Ocean Sea Ice Export Between Nares Strait and the Canadian Arctic Archipelago |
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