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 Tallurutiup Imanga, 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 p...

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Published in:Remote Sensing
Main Author: R.F. Vincent
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2023
Subjects:
Online Access:https://doi.org/10.3390/rs15040954
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spelling ftmdpi:oai:mdpi.com:/2072-4292/15/4/954/ 2023-08-20T04:04:58+02:00 An Assessment of the Lancaster Sound Polynya Using Satellite Data 1979 to 2022 R.F. Vincent agris 2023-02-09 application/pdf https://doi.org/10.3390/rs15040954 EN eng Multidisciplinary Digital Publishing Institute Environmental Remote Sensing https://dx.doi.org/10.3390/rs15040954 https://creativecommons.org/licenses/by/4.0/ Remote Sensing; Volume 15; Issue 4; Pages: 954 remote sensing arctic waters Lancaster Sound polynya ice arch sea ice AVHRR sea surface temperature ice surface temperature Text 2023 ftmdpi https://doi.org/10.3390/rs15040954 2023-08-01T08:43:32Z Situated between Devon Island and Baffin Island, Lancaster Sound is part of Tallurutiup Imanga, 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 km2 and 40,000 km2. 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. Text Arctic Baffin Island Baffin Devon Island Lancaster Sound Northwest passage Sea ice MDPI Open Access Publishing Arctic Baffin Island Canada Northwest Passage Devon Island ENVELOPE(-88.000,-88.000,75.252,75.252) Lancaster Sound ENVELOPE(-83.999,-83.999,74.218,74.218) Remote Sensing 15 4 954
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic remote sensing
arctic waters
Lancaster Sound
polynya
ice arch
sea ice
AVHRR
sea surface temperature
ice surface temperature
spellingShingle remote sensing
arctic waters
Lancaster Sound
polynya
ice arch
sea ice
AVHRR
sea surface temperature
ice surface temperature
R.F. Vincent
An Assessment of the Lancaster Sound Polynya Using Satellite Data 1979 to 2022
topic_facet remote sensing
arctic waters
Lancaster Sound
polynya
ice arch
sea ice
AVHRR
sea surface temperature
ice surface temperature
description Situated between Devon Island and Baffin Island, Lancaster Sound is part of Tallurutiup Imanga, 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 km2 and 40,000 km2. 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.
format Text
author R.F. Vincent
author_facet R.F. Vincent
author_sort R.F. Vincent
title 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_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_sort assessment of the lancaster sound polynya using satellite data 1979 to 2022
publisher Multidisciplinary Digital Publishing Institute
publishDate 2023
url https://doi.org/10.3390/rs15040954
op_coverage agris
long_lat ENVELOPE(-88.000,-88.000,75.252,75.252)
ENVELOPE(-83.999,-83.999,74.218,74.218)
geographic Arctic
Baffin Island
Canada
Northwest Passage
Devon Island
Lancaster Sound
geographic_facet Arctic
Baffin Island
Canada
Northwest Passage
Devon Island
Lancaster Sound
genre Arctic
Baffin Island
Baffin
Devon Island
Lancaster Sound
Northwest passage
Sea ice
genre_facet Arctic
Baffin Island
Baffin
Devon Island
Lancaster Sound
Northwest passage
Sea ice
op_source Remote Sensing; Volume 15; Issue 4; Pages: 954
op_relation Environmental Remote Sensing
https://dx.doi.org/10.3390/rs15040954
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/rs15040954
container_title Remote Sensing
container_volume 15
container_issue 4
container_start_page 954
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