Shoreline changes in eastern Parry Peninsula, Amundsen Gulf, Canada
As the Arctic warms, permafrost coasts are eroding faster, threatening coastal communities, habitats, and altering sediment and nutrient budgets. The western Canadian Arctic is eroding at a rapid pace, however little is known on changes occurring in the in the Amundsen Bay area. This study was condu...
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ftzenodo:oai:zenodo.org:7572256 2024-09-15T17:38:52+00:00 Shoreline changes in eastern Parry Peninsula, Amundsen Gulf, Canada Tanguy, Rodrigue Whalen, Dustin Prates, Gonçalo Vieira, Gonçalo 2023-01-26 https://doi.org/10.5281/zenodo.7572256 unknown Zenodo https://zenodo.org/communities/eu https://doi.org/10.5281/zenodo.7572255 https://doi.org/10.5281/zenodo.7572256 oai:zenodo.org:7572256 info:eu-repo/semantics/openAccess Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode Coastal dynamics Permafrost Darnley Bay Carbon fluxes Remote sensing info:eu-repo/semantics/article 2023 ftzenodo https://doi.org/10.5281/zenodo.757225610.5281/zenodo.7572255 2024-07-26T21:29:08Z As the Arctic warms, permafrost coasts are eroding faster, threatening coastal communities, habitats, and altering sediment and nutrient budgets. The western Canadian Arctic is eroding at a rapid pace, however little is known on changes occurring in the in the Amundsen Bay area. This study was conducted in the eastern coast of Parry Peninsula, a neglected rocky coastal area. We used orthorectified aerial photos of 1965 and 1993 and very-high resolution satellite imagery of 2020 to manually delineate the shoreline and classify the backshore and foreshore typology. Shoreline change rates were calculated and the ArctiDEM was used to derive cliff height, allowing for estimating volume changes and soil organic carbon fluxes. The results show a mean rate of 0.13 m/yr for the backshore zone and 0.2 m/yr for the foreshore, with increasing erosion in the south sector of the Peninsula in the recent decades. The average sediment flux was 19 m 3 /m/yr and The SOC flux 6.7 kg C/m/yr. We highlight the importance of using the clifftop as shoreline reference to accurately estimate sediment fluxes, an approach that is neglected in automatic shoreline delineation techniques based on remote sensing imagery, which generally focus on the identification of the waterline. Article in Journal/Newspaper Amundsen Bay Amundsen Gulf Darnley Bay Parry Peninsula permafrost Zenodo |
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Coastal dynamics Permafrost Darnley Bay Carbon fluxes Remote sensing |
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Coastal dynamics Permafrost Darnley Bay Carbon fluxes Remote sensing Tanguy, Rodrigue Whalen, Dustin Prates, Gonçalo Vieira, Gonçalo Shoreline changes in eastern Parry Peninsula, Amundsen Gulf, Canada |
topic_facet |
Coastal dynamics Permafrost Darnley Bay Carbon fluxes Remote sensing |
description |
As the Arctic warms, permafrost coasts are eroding faster, threatening coastal communities, habitats, and altering sediment and nutrient budgets. The western Canadian Arctic is eroding at a rapid pace, however little is known on changes occurring in the in the Amundsen Bay area. This study was conducted in the eastern coast of Parry Peninsula, a neglected rocky coastal area. We used orthorectified aerial photos of 1965 and 1993 and very-high resolution satellite imagery of 2020 to manually delineate the shoreline and classify the backshore and foreshore typology. Shoreline change rates were calculated and the ArctiDEM was used to derive cliff height, allowing for estimating volume changes and soil organic carbon fluxes. The results show a mean rate of 0.13 m/yr for the backshore zone and 0.2 m/yr for the foreshore, with increasing erosion in the south sector of the Peninsula in the recent decades. The average sediment flux was 19 m 3 /m/yr and The SOC flux 6.7 kg C/m/yr. We highlight the importance of using the clifftop as shoreline reference to accurately estimate sediment fluxes, an approach that is neglected in automatic shoreline delineation techniques based on remote sensing imagery, which generally focus on the identification of the waterline. |
format |
Article in Journal/Newspaper |
author |
Tanguy, Rodrigue Whalen, Dustin Prates, Gonçalo Vieira, Gonçalo |
author_facet |
Tanguy, Rodrigue Whalen, Dustin Prates, Gonçalo Vieira, Gonçalo |
author_sort |
Tanguy, Rodrigue |
title |
Shoreline changes in eastern Parry Peninsula, Amundsen Gulf, Canada |
title_short |
Shoreline changes in eastern Parry Peninsula, Amundsen Gulf, Canada |
title_full |
Shoreline changes in eastern Parry Peninsula, Amundsen Gulf, Canada |
title_fullStr |
Shoreline changes in eastern Parry Peninsula, Amundsen Gulf, Canada |
title_full_unstemmed |
Shoreline changes in eastern Parry Peninsula, Amundsen Gulf, Canada |
title_sort |
shoreline changes in eastern parry peninsula, amundsen gulf, canada |
publisher |
Zenodo |
publishDate |
2023 |
url |
https://doi.org/10.5281/zenodo.7572256 |
genre |
Amundsen Bay Amundsen Gulf Darnley Bay Parry Peninsula permafrost |
genre_facet |
Amundsen Bay Amundsen Gulf Darnley Bay Parry Peninsula permafrost |
op_relation |
https://zenodo.org/communities/eu https://doi.org/10.5281/zenodo.7572255 https://doi.org/10.5281/zenodo.7572256 oai:zenodo.org:7572256 |
op_rights |
info:eu-repo/semantics/openAccess Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode |
op_doi |
https://doi.org/10.5281/zenodo.757225610.5281/zenodo.7572255 |
_version_ |
1810475829357969408 |