Where and Why Do Coastal Retrogressive Thaw Slumps Develop?

Retrogressive thaw slumps (RTSs) are among the most active landforms in the Arctic; their number has increased tremendously over the past decades. While processes initiating discrete RTSs are well defined, little research has been done on a regional scale to reveal the major terrain controls on thei...

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Main Authors: Ramage, Justine, Irrgang, Anna, Morgenstern, Anne, Herzschuh, Ulrike, Couture, N., Lantuit, Hugues
Format: Conference Object
Language:unknown
Published: 2016
Subjects:
Online Access:https://epic.awi.de/id/eprint/43436/
https://epic.awi.de/id/eprint/43436/1/AGU_poster_JustineRamage.pdf
https://hdl.handle.net/10013/epic.49880
https://hdl.handle.net/10013/epic.49880.d001
id ftawi:oai:epic.awi.de:43436
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spelling ftawi:oai:epic.awi.de:43436 2024-09-09T19:26:42+00:00 Where and Why Do Coastal Retrogressive Thaw Slumps Develop? Ramage, Justine Irrgang, Anna Morgenstern, Anne Herzschuh, Ulrike Couture, N. Lantuit, Hugues 2016-12-09 application/pdf https://epic.awi.de/id/eprint/43436/ https://epic.awi.de/id/eprint/43436/1/AGU_poster_JustineRamage.pdf https://hdl.handle.net/10013/epic.49880 https://hdl.handle.net/10013/epic.49880.d001 unknown https://epic.awi.de/id/eprint/43436/1/AGU_poster_JustineRamage.pdf https://hdl.handle.net/10013/epic.49880.d001 Ramage, J. , Irrgang, A. orcid:0000-0002-8158-9675 , Morgenstern, A. orcid:0000-0002-6466-7571 , Herzschuh, U. orcid:0000-0003-0999-1261 , Couture, N. and Lantuit, H. orcid:0000-0003-1497-6760 (2016) Where and Why Do Coastal Retrogressive Thaw Slumps Develop? , AGU, 12 December 2016 - 16 December 2016 . hdl:10013/epic.49880 EPIC3AGU, 2016-12-12-2016-12-16 Conference notRev 2016 ftawi 2024-06-24T04:16:35Z Retrogressive thaw slumps (RTSs) are among the most active landforms in the Arctic; their number has increased tremendously over the past decades. While processes initiating discrete RTSs are well defined, little research has been done on a regional scale to reveal the major terrain controls on their development. Our research provides new insights into the dynamics of coastal RTSs. We reveal the main geomorphic factors determining the development of RTSs along a 238 km coastal segment of the Yukon Coastal Plain, Canada. We 1) show the current extent of RTSs, 2) ascertain the factors controlling their activity and initiation, and 3) explain the differences in density and coverage of RTSs. We mapped and classified the RTSs based on high-resolution satellite images acquired in 2011. We derived the terrain characteristics for each RTS and highlighted the main terrain controls over their development using univariate regression trees. We tested the response variables (RTSs activity, initiation, density and coverage) against 16 environmental variables. We detected 287 coastal RTSs in the study area. Both the activity and the initiation of the RTSs were influenced by coastal geomorphology: active RTSs and new RTSs occurred primarily on terrain with slope angles greater than 3.9° and 5.9°, respectively. The density and coverage of RTSs within each coastal segment were constrained by the volume and thickness of massive ice bodies. Coastal erosion appears to have only an indirect effect on the development of RTSs by maintaining the best conditions for RTSs to reactivate. Conference Object Arctic Yukon Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) Arctic Canada Yukon
institution Open Polar
collection Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center)
op_collection_id ftawi
language unknown
description Retrogressive thaw slumps (RTSs) are among the most active landforms in the Arctic; their number has increased tremendously over the past decades. While processes initiating discrete RTSs are well defined, little research has been done on a regional scale to reveal the major terrain controls on their development. Our research provides new insights into the dynamics of coastal RTSs. We reveal the main geomorphic factors determining the development of RTSs along a 238 km coastal segment of the Yukon Coastal Plain, Canada. We 1) show the current extent of RTSs, 2) ascertain the factors controlling their activity and initiation, and 3) explain the differences in density and coverage of RTSs. We mapped and classified the RTSs based on high-resolution satellite images acquired in 2011. We derived the terrain characteristics for each RTS and highlighted the main terrain controls over their development using univariate regression trees. We tested the response variables (RTSs activity, initiation, density and coverage) against 16 environmental variables. We detected 287 coastal RTSs in the study area. Both the activity and the initiation of the RTSs were influenced by coastal geomorphology: active RTSs and new RTSs occurred primarily on terrain with slope angles greater than 3.9° and 5.9°, respectively. The density and coverage of RTSs within each coastal segment were constrained by the volume and thickness of massive ice bodies. Coastal erosion appears to have only an indirect effect on the development of RTSs by maintaining the best conditions for RTSs to reactivate.
format Conference Object
author Ramage, Justine
Irrgang, Anna
Morgenstern, Anne
Herzschuh, Ulrike
Couture, N.
Lantuit, Hugues
spellingShingle Ramage, Justine
Irrgang, Anna
Morgenstern, Anne
Herzschuh, Ulrike
Couture, N.
Lantuit, Hugues
Where and Why Do Coastal Retrogressive Thaw Slumps Develop?
author_facet Ramage, Justine
Irrgang, Anna
Morgenstern, Anne
Herzschuh, Ulrike
Couture, N.
Lantuit, Hugues
author_sort Ramage, Justine
title Where and Why Do Coastal Retrogressive Thaw Slumps Develop?
title_short Where and Why Do Coastal Retrogressive Thaw Slumps Develop?
title_full Where and Why Do Coastal Retrogressive Thaw Slumps Develop?
title_fullStr Where and Why Do Coastal Retrogressive Thaw Slumps Develop?
title_full_unstemmed Where and Why Do Coastal Retrogressive Thaw Slumps Develop?
title_sort where and why do coastal retrogressive thaw slumps develop?
publishDate 2016
url https://epic.awi.de/id/eprint/43436/
https://epic.awi.de/id/eprint/43436/1/AGU_poster_JustineRamage.pdf
https://hdl.handle.net/10013/epic.49880
https://hdl.handle.net/10013/epic.49880.d001
geographic Arctic
Canada
Yukon
geographic_facet Arctic
Canada
Yukon
genre Arctic
Yukon
genre_facet Arctic
Yukon
op_source EPIC3AGU, 2016-12-12-2016-12-16
op_relation https://epic.awi.de/id/eprint/43436/1/AGU_poster_JustineRamage.pdf
https://hdl.handle.net/10013/epic.49880.d001
Ramage, J. , Irrgang, A. orcid:0000-0002-8158-9675 , Morgenstern, A. orcid:0000-0002-6466-7571 , Herzschuh, U. orcid:0000-0003-0999-1261 , Couture, N. and Lantuit, H. orcid:0000-0003-1497-6760 (2016) Where and Why Do Coastal Retrogressive Thaw Slumps Develop? , AGU, 12 December 2016 - 16 December 2016 . hdl:10013/epic.49880
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