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: J. L. Ramage, A. M. Irrgang, A. Morgenstern, H. Lantuit
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2018
Subjects:
Online Access:https://doi.org/10.5194/bg-15-1483-2018
https://doaj.org/article/8ee6580543ce41558bb550d1b1751d3d
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spelling ftdoajarticles:oai:doaj.org/article:8ee6580543ce41558bb550d1b1751d3d 2023-05-15T14:52:02+02:00 Increasing coastal slump activity impacts the release of sediment and organic carbon into the Arctic Ocean J. L. Ramage A. M. Irrgang A. Morgenstern H. Lantuit 2018-03-01T00:00:00Z https://doi.org/10.5194/bg-15-1483-2018 https://doaj.org/article/8ee6580543ce41558bb550d1b1751d3d EN eng Copernicus Publications https://www.biogeosciences.net/15/1483/2018/bg-15-1483-2018.pdf https://doaj.org/toc/1726-4170 https://doaj.org/toc/1726-4189 doi:10.5194/bg-15-1483-2018 1726-4170 1726-4189 https://doaj.org/article/8ee6580543ce41558bb550d1b1751d3d Biogeosciences, Vol 15, Pp 1483-1495 (2018) Ecology QH540-549.5 Life QH501-531 Geology QE1-996.5 article 2018 ftdoajarticles https://doi.org/10.5194/bg-15-1483-2018 2022-12-31T13:30:41Z 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 16.6×10 6 m 3 of material, 53 % of which was ice, and mobilized 145.9×10 6 kg of OC. Between 1972 and 2011, 49 RTSs displaced 8.6×10 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 Directory of Open Access Journals: DOAJ Articles Arctic Arctic Ocean Yukon Canada Biogeosciences 15 5 1483 1495
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Ecology
QH540-549.5
Life
QH501-531
Geology
QE1-996.5
spellingShingle Ecology
QH540-549.5
Life
QH501-531
Geology
QE1-996.5
J. L. Ramage
A. M. Irrgang
A. Morgenstern
H. Lantuit
Increasing coastal slump activity impacts the release of sediment and organic carbon into the Arctic Ocean
topic_facet Ecology
QH540-549.5
Life
QH501-531
Geology
QE1-996.5
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 16.6×10 6 m 3 of material, 53 % of which was ice, and mobilized 145.9×10 6 kg of OC. Between 1972 and 2011, 49 RTSs displaced 8.6×10 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
author J. L. Ramage
A. M. Irrgang
A. Morgenstern
H. Lantuit
author_facet J. L. Ramage
A. M. Irrgang
A. Morgenstern
H. Lantuit
author_sort J. L. Ramage
title 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_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_sort increasing coastal slump activity impacts the release of sediment and organic carbon into the arctic ocean
publisher Copernicus Publications
publishDate 2018
url https://doi.org/10.5194/bg-15-1483-2018
https://doaj.org/article/8ee6580543ce41558bb550d1b1751d3d
geographic Arctic
Arctic Ocean
Yukon
Canada
geographic_facet Arctic
Arctic Ocean
Yukon
Canada
genre Arctic
Arctic Ocean
Thermokarst
Yukon
genre_facet Arctic
Arctic Ocean
Thermokarst
Yukon
op_source Biogeosciences, Vol 15, Pp 1483-1495 (2018)
op_relation https://www.biogeosciences.net/15/1483/2018/bg-15-1483-2018.pdf
https://doaj.org/toc/1726-4170
https://doaj.org/toc/1726-4189
doi:10.5194/bg-15-1483-2018
1726-4170
1726-4189
https://doaj.org/article/8ee6580543ce41558bb550d1b1751d3d
op_doi https://doi.org/10.5194/bg-15-1483-2018
container_title Biogeosciences
container_volume 15
container_issue 5
container_start_page 1483
op_container_end_page 1495
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