Satellite-Based Evaluation of Submarine Permafrost Erosion at Shallow Offshore Areas in the Laptev Sea

Large areas of the seafloor in the Laptev Sea consist of submarine permafrost, which has experienced intense degradation over the last decades and centuries. Thermal abrasion of the submarine permafrost results in upward advection of suspended matter, which could reach the surface layer in shallow a...

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Published in:Remote Sensing
Main Authors: Alexander Osadchiev, Polina Adamovskaya, Stanislav Myslenkov, Oleg Dudarev, Igor Semiletov
Format: Article in Journal/Newspaper
Language:English
Published: MDPI AG 2023
Subjects:
Q
Ice
Online Access:https://doi.org/10.3390/rs15205065
https://doaj.org/article/53fb5f128bbd4c6bbbda5293d8c29178
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spelling ftdoajarticles:oai:doaj.org/article:53fb5f128bbd4c6bbbda5293d8c29178 2023-11-12T04:18:25+01:00 Satellite-Based Evaluation of Submarine Permafrost Erosion at Shallow Offshore Areas in the Laptev Sea Alexander Osadchiev Polina Adamovskaya Stanislav Myslenkov Oleg Dudarev Igor Semiletov 2023-10-01T00:00:00Z https://doi.org/10.3390/rs15205065 https://doaj.org/article/53fb5f128bbd4c6bbbda5293d8c29178 EN eng MDPI AG https://www.mdpi.com/2072-4292/15/20/5065 https://doaj.org/toc/2072-4292 doi:10.3390/rs15205065 2072-4292 https://doaj.org/article/53fb5f128bbd4c6bbbda5293d8c29178 Remote Sensing, Vol 15, Iss 5065, p 5065 (2023) bottom sediments coastal upwelling seafloor erosion submarine permafrost thermal abrasion suspended matter flux Science Q article 2023 ftdoajarticles https://doi.org/10.3390/rs15205065 2023-10-29T00:35:45Z Large areas of the seafloor in the Laptev Sea consist of submarine permafrost, which has experienced intense degradation over the last decades and centuries. Thermal abrasion of the submarine permafrost results in upward advection of suspended matter, which could reach the surface layer in shallow areas. This process is visually manifested through increased turbidity of the sea surface layer, which is regularly detected in optical satellite imagery of the study areas. In this study, satellite data, wind and wave reanalysis, as well as in situ measurements are analyzed in order to reveal the main mechanisms of seafloor erosion in shallow areas of the Laptev Sea. We describe the synoptic variability in erosion at the Vasilyevskaya and Semenovskaya shoals in response to wind and wave conditions. Finally, using reanalysis data, daily suspended matter flux from this area was evaluated during ice-free periods in 1979–2021, and its seasonal and inter-annual variabilities were described. The obtained results contribute to our understanding of subsea permafrost degradation, the sediment budget, and carbon and nutrient cycles in the Laptev Sea. Article in Journal/Newspaper Ice laptev Laptev Sea permafrost Directory of Open Access Journals: DOAJ Articles Remote Sensing 15 20 5065
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic bottom sediments
coastal upwelling
seafloor erosion
submarine permafrost
thermal abrasion
suspended matter flux
Science
Q
spellingShingle bottom sediments
coastal upwelling
seafloor erosion
submarine permafrost
thermal abrasion
suspended matter flux
Science
Q
Alexander Osadchiev
Polina Adamovskaya
Stanislav Myslenkov
Oleg Dudarev
Igor Semiletov
Satellite-Based Evaluation of Submarine Permafrost Erosion at Shallow Offshore Areas in the Laptev Sea
topic_facet bottom sediments
coastal upwelling
seafloor erosion
submarine permafrost
thermal abrasion
suspended matter flux
Science
Q
description Large areas of the seafloor in the Laptev Sea consist of submarine permafrost, which has experienced intense degradation over the last decades and centuries. Thermal abrasion of the submarine permafrost results in upward advection of suspended matter, which could reach the surface layer in shallow areas. This process is visually manifested through increased turbidity of the sea surface layer, which is regularly detected in optical satellite imagery of the study areas. In this study, satellite data, wind and wave reanalysis, as well as in situ measurements are analyzed in order to reveal the main mechanisms of seafloor erosion in shallow areas of the Laptev Sea. We describe the synoptic variability in erosion at the Vasilyevskaya and Semenovskaya shoals in response to wind and wave conditions. Finally, using reanalysis data, daily suspended matter flux from this area was evaluated during ice-free periods in 1979–2021, and its seasonal and inter-annual variabilities were described. The obtained results contribute to our understanding of subsea permafrost degradation, the sediment budget, and carbon and nutrient cycles in the Laptev Sea.
format Article in Journal/Newspaper
author Alexander Osadchiev
Polina Adamovskaya
Stanislav Myslenkov
Oleg Dudarev
Igor Semiletov
author_facet Alexander Osadchiev
Polina Adamovskaya
Stanislav Myslenkov
Oleg Dudarev
Igor Semiletov
author_sort Alexander Osadchiev
title Satellite-Based Evaluation of Submarine Permafrost Erosion at Shallow Offshore Areas in the Laptev Sea
title_short Satellite-Based Evaluation of Submarine Permafrost Erosion at Shallow Offshore Areas in the Laptev Sea
title_full Satellite-Based Evaluation of Submarine Permafrost Erosion at Shallow Offshore Areas in the Laptev Sea
title_fullStr Satellite-Based Evaluation of Submarine Permafrost Erosion at Shallow Offshore Areas in the Laptev Sea
title_full_unstemmed Satellite-Based Evaluation of Submarine Permafrost Erosion at Shallow Offshore Areas in the Laptev Sea
title_sort satellite-based evaluation of submarine permafrost erosion at shallow offshore areas in the laptev sea
publisher MDPI AG
publishDate 2023
url https://doi.org/10.3390/rs15205065
https://doaj.org/article/53fb5f128bbd4c6bbbda5293d8c29178
genre Ice
laptev
Laptev Sea
permafrost
genre_facet Ice
laptev
Laptev Sea
permafrost
op_source Remote Sensing, Vol 15, Iss 5065, p 5065 (2023)
op_relation https://www.mdpi.com/2072-4292/15/20/5065
https://doaj.org/toc/2072-4292
doi:10.3390/rs15205065
2072-4292
https://doaj.org/article/53fb5f128bbd4c6bbbda5293d8c29178
op_doi https://doi.org/10.3390/rs15205065
container_title Remote Sensing
container_volume 15
container_issue 20
container_start_page 5065
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