Shoreline change rates and land to sea sediment and soil organic carbon transfer in eastern Parry Peninsula from 1965 to 2020 (Amundsen Gulf, Canada)

As the Arctic is warming, 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 Amundsen Gulf area. This study was condu...

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Published in:Arctic Science
Main Authors: Tanguy, Rodrigue, Whalen, Dustin, Prates, Gonçalo, Vieira, Gonçalo
Format: Article in Journal/Newspaper
Language:English
Published: Canadian Science Publishing 2023
Subjects:
Ice
Online Access:http://hdl.handle.net/10400.1/19403
https://doi.org/10.1139/AS-2022-0028
id ftunivalgarve:oai:sapientia.ualg.pt:10400.1/19403
record_format openpolar
spelling ftunivalgarve:oai:sapientia.ualg.pt:10400.1/19403 2023-05-15T13:22:53+02:00 Shoreline change rates and land to sea sediment and soil organic carbon transfer in eastern Parry Peninsula from 1965 to 2020 (Amundsen Gulf, Canada) Tanguy, Rodrigue Whalen, Dustin Prates, Gonçalo Vieira, Gonçalo 2023 http://hdl.handle.net/10400.1/19403 https://doi.org/10.1139/AS-2022-0028 eng eng Canadian Science Publishing info:eu-repo/grantAgreement/EC/H2020/773421/EU http://hdl.handle.net/10400.1/19403 doi:10.1139/AS-2022-0028 2368-7460 openAccess http://creativecommons.org/licenses/by/4.0/ Coastal dynamics Permafrost Darnley Bay Carbon fluxes Remote sensing article 2023 ftunivalgarve https://doi.org/10.1139/AS-2022-0028 2023-04-12T00:06:22Z As the Arctic is warming, 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 Amundsen Gulf area. This study was conducted in the eastern coast of Parry Peninsula, a neglected rock dominated coastal area. We used orthorectified aerial photos of 1965 and 1993 and very high-resolution satellite imagery of 2020 to manually delineate the shoreline according to backshore and foreshore centered approaches. Shoreline change rates were calculated and sediment and organic carbon transfer from land to sea estimated using digital elevation model, the Northern Circumpolar Soil Carbon Database, and ground ice content. The results show a mean erosion rate of 0.12 m/yr for the backshore zone and 0.16 m/yr for the foreshore zone, with increasing erosion in the Paulatuk Peninsula in recent decades. The average sediment transfer from land to sea was 20 m3/m/yr and the soil organic carbon (SOC) flux was 7 kg C/m/yr. We highlight the importance of using the cliff-top as shoreline reference to accurately estimate sediment and SOC transfers, an approach neglected in automatic shoreline delineation techniques based on remote sensing imagery using the waterline. Natural Resources Canada; Canadian Forest Service; Climate Change Geoscience Program, Crown-Indigenous Relations and Northern Affairs Canada (CIRNAC) through the Beaufort Sea; Regional Strategic Environment and Research Assessment (BRSEA); European Union's Horizon 2020 Research and Innovation Program; Community of Paulatuk info:eu-repo/semantics/publishedVersion Article in Journal/Newspaper Amundsen Gulf Arctic Beaufort Sea Climate change Darnley Bay Ice Parry Peninsula Paulatuk permafrost Universidade do Algarve: Sapienta Arctic Canada Darnley ENVELOPE(69.717,69.717,-67.717,-67.717) Darnley Bay ENVELOPE(-123.671,-123.671,69.584,69.584) Parry ENVELOPE(-62.417,-62.417,-64.283,-64.283) Parry Peninsula ENVELOPE(-30.000,-30.000,-79.500,-79.500) Paulatuk ENVELOPE(-123.985,-123.985,69.325,69.325) Arctic Science
institution Open Polar
collection Universidade do Algarve: Sapienta
op_collection_id ftunivalgarve
language English
topic Coastal dynamics
Permafrost
Darnley Bay
Carbon fluxes
Remote sensing
spellingShingle Coastal dynamics
Permafrost
Darnley Bay
Carbon fluxes
Remote sensing
Tanguy, Rodrigue
Whalen, Dustin
Prates, Gonçalo
Vieira, Gonçalo
Shoreline change rates and land to sea sediment and soil organic carbon transfer in eastern Parry Peninsula from 1965 to 2020 (Amundsen Gulf, Canada)
topic_facet Coastal dynamics
Permafrost
Darnley Bay
Carbon fluxes
Remote sensing
description As the Arctic is warming, 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 Amundsen Gulf area. This study was conducted in the eastern coast of Parry Peninsula, a neglected rock dominated coastal area. We used orthorectified aerial photos of 1965 and 1993 and very high-resolution satellite imagery of 2020 to manually delineate the shoreline according to backshore and foreshore centered approaches. Shoreline change rates were calculated and sediment and organic carbon transfer from land to sea estimated using digital elevation model, the Northern Circumpolar Soil Carbon Database, and ground ice content. The results show a mean erosion rate of 0.12 m/yr for the backshore zone and 0.16 m/yr for the foreshore zone, with increasing erosion in the Paulatuk Peninsula in recent decades. The average sediment transfer from land to sea was 20 m3/m/yr and the soil organic carbon (SOC) flux was 7 kg C/m/yr. We highlight the importance of using the cliff-top as shoreline reference to accurately estimate sediment and SOC transfers, an approach neglected in automatic shoreline delineation techniques based on remote sensing imagery using the waterline. Natural Resources Canada; Canadian Forest Service; Climate Change Geoscience Program, Crown-Indigenous Relations and Northern Affairs Canada (CIRNAC) through the Beaufort Sea; Regional Strategic Environment and Research Assessment (BRSEA); European Union's Horizon 2020 Research and Innovation Program; Community of Paulatuk info:eu-repo/semantics/publishedVersion
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 change rates and land to sea sediment and soil organic carbon transfer in eastern Parry Peninsula from 1965 to 2020 (Amundsen Gulf, Canada)
title_short Shoreline change rates and land to sea sediment and soil organic carbon transfer in eastern Parry Peninsula from 1965 to 2020 (Amundsen Gulf, Canada)
title_full Shoreline change rates and land to sea sediment and soil organic carbon transfer in eastern Parry Peninsula from 1965 to 2020 (Amundsen Gulf, Canada)
title_fullStr Shoreline change rates and land to sea sediment and soil organic carbon transfer in eastern Parry Peninsula from 1965 to 2020 (Amundsen Gulf, Canada)
title_full_unstemmed Shoreline change rates and land to sea sediment and soil organic carbon transfer in eastern Parry Peninsula from 1965 to 2020 (Amundsen Gulf, Canada)
title_sort shoreline change rates and land to sea sediment and soil organic carbon transfer in eastern parry peninsula from 1965 to 2020 (amundsen gulf, canada)
publisher Canadian Science Publishing
publishDate 2023
url http://hdl.handle.net/10400.1/19403
https://doi.org/10.1139/AS-2022-0028
long_lat ENVELOPE(69.717,69.717,-67.717,-67.717)
ENVELOPE(-123.671,-123.671,69.584,69.584)
ENVELOPE(-62.417,-62.417,-64.283,-64.283)
ENVELOPE(-30.000,-30.000,-79.500,-79.500)
ENVELOPE(-123.985,-123.985,69.325,69.325)
geographic Arctic
Canada
Darnley
Darnley Bay
Parry
Parry Peninsula
Paulatuk
geographic_facet Arctic
Canada
Darnley
Darnley Bay
Parry
Parry Peninsula
Paulatuk
genre Amundsen Gulf
Arctic
Beaufort Sea
Climate change
Darnley Bay
Ice
Parry Peninsula
Paulatuk
permafrost
genre_facet Amundsen Gulf
Arctic
Beaufort Sea
Climate change
Darnley Bay
Ice
Parry Peninsula
Paulatuk
permafrost
op_relation info:eu-repo/grantAgreement/EC/H2020/773421/EU
http://hdl.handle.net/10400.1/19403
doi:10.1139/AS-2022-0028
2368-7460
op_rights openAccess
http://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.1139/AS-2022-0028
container_title Arctic Science
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