An Assessment of the Lancaster Sound Polynya Using Satellite Data 1979 to 2022
Situated between Devon Island and Baffin Island, Lancaster Sound is part of <i>Tallurutiup Imanga</i>, which is in the process of becoming the largest marine conservation area in Canada. The cultural and ecological significance of the region is due, in part, to a recurring polynya in Lan...
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| Format: | Article |
| Language: | English |
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MDPI AG
2023-02-01
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| Series: | Remote Sensing |
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| Online Access: | https://www.mdpi.com/2072-4292/15/4/954 |
| _version_ | 1797618417320067072 |
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| author | R.F. Vincent |
| author_facet | R.F. Vincent |
| author_sort | R.F. Vincent |
| collection | DOAJ |
| description | Situated between Devon Island and Baffin Island, Lancaster Sound is part of <i>Tallurutiup Imanga</i>, which is in the process of becoming the largest marine conservation area in Canada. The cultural and ecological significance of the region is due, in part, to a recurring polynya in Lancaster Sound. The polynya is demarcated by an ice arch that generally forms in mid-winter and collapses in late spring or early summer. Advanced Very High Resolution imagery from 1979 to 2022 was analyzed to determine the position, formation and collapse of the Lancaster Sound ice arch. The location of the ice arch demonstrates high interannual variability, with 512 km between the eastern and western extremes, resulting in a polynya area that can fluctuate between 6000 km<sup>2</sup> and 40,000 km<sup>2</sup>. The timing of the seasonal ice arch formation and collapse has implications with respect to ice transport through Lancaster Sound and the navigability of the Northwest Passage. The date of both the formation and collapse of the ice arch is variable from season to season, with the formation observed between November and April and collapse usually occurring in June or July. A linear trend from 1979 to 2022 indicates that seasonal ice arch duration has declined from 150 to 102 days. The reduction in ice arch duration is a result of earlier collapse dates over the study period and later formation dates, particularly from 1979 to 2000. Lancaster Sound normally freezes west to east each season until the ice arch is established, but there is no statistical relationship between the ice arch location and duration. Satellite surface temperature mapping of the region indicates that the polynya is characterized by sub-resolution leads during winter. |
| first_indexed | 2024-03-11T08:12:36Z |
| format | Article |
| id | doaj.art-2e0c4e5729434f7e91e03ee51f93853e |
| institution | Directory Open Access Journal |
| issn | 2072-4292 |
| language | English |
| last_indexed | 2024-03-11T08:12:36Z |
| publishDate | 2023-02-01 |
| publisher | MDPI AG |
| record_format | Article |
| series | Remote Sensing |
| spelling | doaj.art-2e0c4e5729434f7e91e03ee51f93853e2023-11-16T23:01:44ZengMDPI AGRemote Sensing2072-42922023-02-0115495410.3390/rs15040954An Assessment of the Lancaster Sound Polynya Using Satellite Data 1979 to 2022R.F. Vincent0Department of Physics and Space Science, Royal Military College of Canada, Kingston, ON K7K 7B4, CanadaSituated between Devon Island and Baffin Island, Lancaster Sound is part of <i>Tallurutiup Imanga</i>, which is in the process of becoming the largest marine conservation area in Canada. The cultural and ecological significance of the region is due, in part, to a recurring polynya in Lancaster Sound. The polynya is demarcated by an ice arch that generally forms in mid-winter and collapses in late spring or early summer. Advanced Very High Resolution imagery from 1979 to 2022 was analyzed to determine the position, formation and collapse of the Lancaster Sound ice arch. The location of the ice arch demonstrates high interannual variability, with 512 km between the eastern and western extremes, resulting in a polynya area that can fluctuate between 6000 km<sup>2</sup> and 40,000 km<sup>2</sup>. The timing of the seasonal ice arch formation and collapse has implications with respect to ice transport through Lancaster Sound and the navigability of the Northwest Passage. The date of both the formation and collapse of the ice arch is variable from season to season, with the formation observed between November and April and collapse usually occurring in June or July. A linear trend from 1979 to 2022 indicates that seasonal ice arch duration has declined from 150 to 102 days. The reduction in ice arch duration is a result of earlier collapse dates over the study period and later formation dates, particularly from 1979 to 2000. Lancaster Sound normally freezes west to east each season until the ice arch is established, but there is no statistical relationship between the ice arch location and duration. Satellite surface temperature mapping of the region indicates that the polynya is characterized by sub-resolution leads during winter.https://www.mdpi.com/2072-4292/15/4/954remote sensingarctic watersLancaster Soundpolynyaice archsea ice |
| spellingShingle | R.F. Vincent An Assessment of the Lancaster Sound Polynya Using Satellite Data 1979 to 2022 Remote Sensing remote sensing arctic waters Lancaster Sound polynya ice arch sea ice |
| title | An Assessment of the Lancaster Sound Polynya Using Satellite Data 1979 to 2022 |
| title_full | An Assessment of the Lancaster Sound Polynya Using Satellite Data 1979 to 2022 |
| title_fullStr | An Assessment of the Lancaster Sound Polynya Using Satellite Data 1979 to 2022 |
| title_full_unstemmed | An Assessment of the Lancaster Sound Polynya Using Satellite Data 1979 to 2022 |
| title_short | An Assessment of the Lancaster Sound Polynya Using Satellite Data 1979 to 2022 |
| title_sort | assessment of the lancaster sound polynya using satellite data 1979 to 2022 |
| topic | remote sensing arctic waters Lancaster Sound polynya ice arch sea ice |
| url | https://www.mdpi.com/2072-4292/15/4/954 |
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