Long-Term Analysis of Sea Ice Drift in the Western Ross Sea, Antarctica, at High and Low Spatial Resolution

The Ross Sea region, including three main polynya areas in McMurdo Sound, Terra Nova Bay, and in front of the Ross Ice Shelf, has experienced a significant increase in sea ice extent in the first four decades of satellite observations. Here, we use Co-Registration of Optically Sensed Images and Corr...

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Published in:Remote Sensing
Main Authors: Usama Farooq, Wolfgang Rack, Adrian McDonald, Stephen Howell
Format: Article in Journal/Newspaper
Language:English
Published: MDPI AG 2020
Subjects:
Q
Online Access:https://doi.org/10.3390/rs12091402
https://doaj.org/article/9fd0494eb85741fa8cdae52fd5921b0f
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spelling ftdoajarticles:oai:doaj.org/article:9fd0494eb85741fa8cdae52fd5921b0f 2023-05-15T14:04:00+02:00 Long-Term Analysis of Sea Ice Drift in the Western Ross Sea, Antarctica, at High and Low Spatial Resolution Usama Farooq Wolfgang Rack Adrian McDonald Stephen Howell 2020-04-01T00:00:00Z https://doi.org/10.3390/rs12091402 https://doaj.org/article/9fd0494eb85741fa8cdae52fd5921b0f EN eng MDPI AG https://www.mdpi.com/2072-4292/12/9/1402 https://doaj.org/toc/2072-4292 doi:10.3390/rs12091402 2072-4292 https://doaj.org/article/9fd0494eb85741fa8cdae52fd5921b0f Remote Sensing, Vol 12, Iss 1402, p 1402 (2020) sea ice motion tracking Envisat ASAR Polar Pathfinder NSIDC Western Ross Sea Science Q article 2020 ftdoajarticles https://doi.org/10.3390/rs12091402 2022-12-31T16:33:36Z The Ross Sea region, including three main polynya areas in McMurdo Sound, Terra Nova Bay, and in front of the Ross Ice Shelf, has experienced a significant increase in sea ice extent in the first four decades of satellite observations. Here, we use Co-Registration of Optically Sensed Images and Correlation (COSI-Corr) to estimate 894 high-resolution sea ice motion fields of the Western Ross Sea in order to explore ice-atmosphere interactions based on sequential high-resolution Advanced Synthetic Aperture Radar (ASAR) images from the Envisat satellite acquired between 2002–2012. Validation of output motion vectors with manually drawn vectors for 24 image pairs show Pearson correlation coefficients of 0.92 ± 0.09 with a mean deviation in direction of −3.17 ± 6.48 degrees. The high-resolution vectors were also validated against the Environment and Climate Change Canada sea ice motion tracking algorithm, resulting in correlation coefficients of 0.84 ± 0.20 and the mean deviation in the direction of −0.04 ± 17.39 degrees. A total of 480 one-day separated velocity vector fields have been compared to an available NSIDC low-resolution sea ice motion vector product, showing much lower correlations and high directional differences. The high-resolution product is able to better identify short-term and spatial variations, whereas the low-resolution product underestimates the actual sea ice velocities by 47% in this important near-coastal region. The large-scale pattern of sea ice drift over the full time period is similar in both products. Improved image coverage is still desired to capture drift variations shorter than 24 h. Article in Journal/Newspaper Antarc* Antarctica Ice Shelf McMurdo Sound Ross Ice Shelf Ross Sea Sea ice Directory of Open Access Journals: DOAJ Articles Ross Sea McMurdo Sound Terra Nova Bay Ross Ice Shelf Canada Asar ENVELOPE(134.033,134.033,68.667,68.667) Remote Sensing 12 9 1402
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic sea ice
motion tracking
Envisat ASAR
Polar Pathfinder
NSIDC
Western Ross Sea
Science
Q
spellingShingle sea ice
motion tracking
Envisat ASAR
Polar Pathfinder
NSIDC
Western Ross Sea
Science
Q
Usama Farooq
Wolfgang Rack
Adrian McDonald
Stephen Howell
Long-Term Analysis of Sea Ice Drift in the Western Ross Sea, Antarctica, at High and Low Spatial Resolution
topic_facet sea ice
motion tracking
Envisat ASAR
Polar Pathfinder
NSIDC
Western Ross Sea
Science
Q
description The Ross Sea region, including three main polynya areas in McMurdo Sound, Terra Nova Bay, and in front of the Ross Ice Shelf, has experienced a significant increase in sea ice extent in the first four decades of satellite observations. Here, we use Co-Registration of Optically Sensed Images and Correlation (COSI-Corr) to estimate 894 high-resolution sea ice motion fields of the Western Ross Sea in order to explore ice-atmosphere interactions based on sequential high-resolution Advanced Synthetic Aperture Radar (ASAR) images from the Envisat satellite acquired between 2002–2012. Validation of output motion vectors with manually drawn vectors for 24 image pairs show Pearson correlation coefficients of 0.92 ± 0.09 with a mean deviation in direction of −3.17 ± 6.48 degrees. The high-resolution vectors were also validated against the Environment and Climate Change Canada sea ice motion tracking algorithm, resulting in correlation coefficients of 0.84 ± 0.20 and the mean deviation in the direction of −0.04 ± 17.39 degrees. A total of 480 one-day separated velocity vector fields have been compared to an available NSIDC low-resolution sea ice motion vector product, showing much lower correlations and high directional differences. The high-resolution product is able to better identify short-term and spatial variations, whereas the low-resolution product underestimates the actual sea ice velocities by 47% in this important near-coastal region. The large-scale pattern of sea ice drift over the full time period is similar in both products. Improved image coverage is still desired to capture drift variations shorter than 24 h.
format Article in Journal/Newspaper
author Usama Farooq
Wolfgang Rack
Adrian McDonald
Stephen Howell
author_facet Usama Farooq
Wolfgang Rack
Adrian McDonald
Stephen Howell
author_sort Usama Farooq
title Long-Term Analysis of Sea Ice Drift in the Western Ross Sea, Antarctica, at High and Low Spatial Resolution
title_short Long-Term Analysis of Sea Ice Drift in the Western Ross Sea, Antarctica, at High and Low Spatial Resolution
title_full Long-Term Analysis of Sea Ice Drift in the Western Ross Sea, Antarctica, at High and Low Spatial Resolution
title_fullStr Long-Term Analysis of Sea Ice Drift in the Western Ross Sea, Antarctica, at High and Low Spatial Resolution
title_full_unstemmed Long-Term Analysis of Sea Ice Drift in the Western Ross Sea, Antarctica, at High and Low Spatial Resolution
title_sort long-term analysis of sea ice drift in the western ross sea, antarctica, at high and low spatial resolution
publisher MDPI AG
publishDate 2020
url https://doi.org/10.3390/rs12091402
https://doaj.org/article/9fd0494eb85741fa8cdae52fd5921b0f
long_lat ENVELOPE(134.033,134.033,68.667,68.667)
geographic Ross Sea
McMurdo Sound
Terra Nova Bay
Ross Ice Shelf
Canada
Asar
geographic_facet Ross Sea
McMurdo Sound
Terra Nova Bay
Ross Ice Shelf
Canada
Asar
genre Antarc*
Antarctica
Ice Shelf
McMurdo Sound
Ross Ice Shelf
Ross Sea
Sea ice
genre_facet Antarc*
Antarctica
Ice Shelf
McMurdo Sound
Ross Ice Shelf
Ross Sea
Sea ice
op_source Remote Sensing, Vol 12, Iss 1402, p 1402 (2020)
op_relation https://www.mdpi.com/2072-4292/12/9/1402
https://doaj.org/toc/2072-4292
doi:10.3390/rs12091402
2072-4292
https://doaj.org/article/9fd0494eb85741fa8cdae52fd5921b0f
op_doi https://doi.org/10.3390/rs12091402
container_title Remote Sensing
container_volume 12
container_issue 9
container_start_page 1402
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