Increasing coastal slump activity impacts the release of sediment and organic carbon into the Arctic Ocean

Retrogressive thaw slumps (RTSs) are among the most active thermokarst landforms in the Arctic and deliver a large amount of material to the Arctic Ocean. However, their contribution to the organic carbon (OC) budget is unknown. We provide the first estimate of the contribution of RTSs to the nearsh...

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Published in:Biogeosciences
Main Authors: Ramage, Justine Lucille, Irrgang, Anna Maria, Morgenstern, Anne, Lantuit, Hugues (Prof. Dr.)
Format: Article in Journal/Newspaper
Language:English
Published: 2018
Subjects:
Online Access:https://publishup.uni-potsdam.de/frontdoor/index/index/docId/53322
https://doi.org/10.5194/bg-15-1483-2018
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author Ramage, Justine Lucille
Irrgang, Anna Maria
Morgenstern, Anne
Lantuit, Hugues (Prof. Dr.)
author_facet Ramage, Justine Lucille
Irrgang, Anna Maria
Morgenstern, Anne
Lantuit, Hugues (Prof. Dr.)
author_sort Ramage, Justine Lucille
collection University of Potsdam: publish.UP
container_issue 5
container_start_page 1483
container_title Biogeosciences
container_volume 15
description Retrogressive thaw slumps (RTSs) are among the most active thermokarst landforms in the Arctic and deliver a large amount of material to the Arctic Ocean. However, their contribution to the organic carbon (OC) budget is unknown. We provide the first estimate of the contribution of RTSs to the nearshore OC budget of the Yukon Coast, Canada, and describe the evolution of coastal RTSs between 1952 and 2011 in this area. We (1) describe the evolution of RTSs between 1952 and 2011; (2) calculate the volume of eroded material and stocks of OC mobilized through slumping, including soil organic carbon (SOC) and dissolved organic carbon (DOC); and (3) estimate the OC fluxes mobilized through slumping between 1972 and 2011. We identified RTSs using high- resolution satellite imagery from 2011 and geocoded aerial photographs from 1952 and 1972. To estimate the volume of eroded material, we applied spline interpolation on an airborne lidar dataset acquired in July 2013. We inferred the stocks of mobilized SOC and DOC from existing related literature. Our results show a 73% increase in the number of RTSs and 14% areal expansion between 1952 and 2011. In the study area, RTSs displaced at least 16.6 x 10(6) m(3) of material, 53% of which was ice, and mobilized 145.9 x 10(6) kg of OC. Between 1972 and 2011, 49 RTSs displaced 8.6 x 10(3) m(3) yr(-1) of material, adding 0.6% to the OC flux released by coastal retreat along the Yukon Coast. Our results show that the contribution of RTSs to the nearshore OC budget is non-negligible and should be included when estimating the quantity of OC released from the Arctic coast to the ocean.
format Article in Journal/Newspaper
genre Arctic
Arctic Ocean
Thermokarst
Yukon
genre_facet Arctic
Arctic Ocean
Thermokarst
Yukon
geographic Arctic
Arctic Ocean
Canada
Yukon
geographic_facet Arctic
Arctic Ocean
Canada
Yukon
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language English
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op_doi https://doi.org/10.5194/bg-15-1483-2018
op_rights https://creativecommons.org/licenses/by/4.0/
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spelling ftubpotsdam:oai:kobv.de-opus4-uni-potsdam:53322 2025-04-20T14:31:33+00:00 Increasing coastal slump activity impacts the release of sediment and organic carbon into the Arctic Ocean Ramage, Justine Lucille Irrgang, Anna Maria Morgenstern, Anne Lantuit, Hugues (Prof. Dr.) 2018-03-13 https://publishup.uni-potsdam.de/frontdoor/index/index/docId/53322 https://doi.org/10.5194/bg-15-1483-2018 eng eng https://creativecommons.org/licenses/by/4.0/ info:eu-repo/semantics/closedAccess ddc:550 Institut für Geowissenschaften article doc-type:article 2018 ftubpotsdam https://doi.org/10.5194/bg-15-1483-2018 2025-03-25T05:06:46Z Retrogressive thaw slumps (RTSs) are among the most active thermokarst landforms in the Arctic and deliver a large amount of material to the Arctic Ocean. However, their contribution to the organic carbon (OC) budget is unknown. We provide the first estimate of the contribution of RTSs to the nearshore OC budget of the Yukon Coast, Canada, and describe the evolution of coastal RTSs between 1952 and 2011 in this area. We (1) describe the evolution of RTSs between 1952 and 2011; (2) calculate the volume of eroded material and stocks of OC mobilized through slumping, including soil organic carbon (SOC) and dissolved organic carbon (DOC); and (3) estimate the OC fluxes mobilized through slumping between 1972 and 2011. We identified RTSs using high- resolution satellite imagery from 2011 and geocoded aerial photographs from 1952 and 1972. To estimate the volume of eroded material, we applied spline interpolation on an airborne lidar dataset acquired in July 2013. We inferred the stocks of mobilized SOC and DOC from existing related literature. Our results show a 73% increase in the number of RTSs and 14% areal expansion between 1952 and 2011. In the study area, RTSs displaced at least 16.6 x 10(6) m(3) of material, 53% of which was ice, and mobilized 145.9 x 10(6) kg of OC. Between 1972 and 2011, 49 RTSs displaced 8.6 x 10(3) m(3) yr(-1) of material, adding 0.6% to the OC flux released by coastal retreat along the Yukon Coast. Our results show that the contribution of RTSs to the nearshore OC budget is non-negligible and should be included when estimating the quantity of OC released from the Arctic coast to the ocean. Article in Journal/Newspaper Arctic Arctic Ocean Thermokarst Yukon University of Potsdam: publish.UP Arctic Arctic Ocean Canada Yukon Biogeosciences 15 5 1483 1495
spellingShingle ddc:550
Institut für Geowissenschaften
Ramage, Justine Lucille
Irrgang, Anna Maria
Morgenstern, Anne
Lantuit, Hugues (Prof. Dr.)
Increasing coastal slump activity impacts the release of sediment and organic carbon into the Arctic Ocean
title Increasing coastal slump activity impacts the release of sediment and organic carbon into the Arctic Ocean
title_full Increasing coastal slump activity impacts the release of sediment and organic carbon into the Arctic Ocean
title_fullStr Increasing coastal slump activity impacts the release of sediment and organic carbon into the Arctic Ocean
title_full_unstemmed Increasing coastal slump activity impacts the release of sediment and organic carbon into the Arctic Ocean
title_short Increasing coastal slump activity impacts the release of sediment and organic carbon into the Arctic Ocean
title_sort increasing coastal slump activity impacts the release of sediment and organic carbon into the arctic ocean
topic ddc:550
Institut für Geowissenschaften
topic_facet ddc:550
Institut für Geowissenschaften
url https://publishup.uni-potsdam.de/frontdoor/index/index/docId/53322
https://doi.org/10.5194/bg-15-1483-2018