Characteristics and recent dynamics of thermo-erosional features in small catchments of Arctic Siberia

Thermal erosion is a prominent type of permafrost degradation that can lead to rapid changes in ice-rich permafrost landscapes. The process and its resulting landforms such as thermo-erosional gullies are reported to become increasingly active and widespread. (Re-)Activation of thermal erosion impac...

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Main Authors: Morgenstern, Anne, Tarbeeva, Anna, Lebedeva, Lyudmila, Shamov, Vladimir, Inauen, Cornelia
Format: Conference Object
Language:unknown
Published: 2023
Subjects:
Ice
Online Access:https://epic.awi.de/id/eprint/57841/
https://epic.awi.de/id/eprint/57841/1/EUCOP2023-ABSTRACTS_Morgenstern.pdf
https://hdl.handle.net/10013/epic.51798c3f-8d47-4553-8d5b-572260362444
id ftawi:oai:epic.awi.de:57841
record_format openpolar
spelling ftawi:oai:epic.awi.de:57841 2023-07-23T04:16:28+02:00 Characteristics and recent dynamics of thermo-erosional features in small catchments of Arctic Siberia Morgenstern, Anne Tarbeeva, Anna Lebedeva, Lyudmila Shamov, Vladimir Inauen, Cornelia 2023-06-20 application/pdf https://epic.awi.de/id/eprint/57841/ https://epic.awi.de/id/eprint/57841/1/EUCOP2023-ABSTRACTS_Morgenstern.pdf https://hdl.handle.net/10013/epic.51798c3f-8d47-4553-8d5b-572260362444 unknown https://epic.awi.de/id/eprint/57841/1/EUCOP2023-ABSTRACTS_Morgenstern.pdf Morgenstern, A. orcid:0000-0002-6466-7571 , Tarbeeva, A. , Lebedeva, L. , Shamov, V. and Inauen, C. (2023) Characteristics and recent dynamics of thermo-erosional features in small catchments of Arctic Siberia hdl:10013/epic.51798c3f-8d47-4553-8d5b-572260362444 EPIC3 Conference NonPeerReviewed 2023 ftawi 2023-07-02T23:19:31Z Thermal erosion is a prominent type of permafrost degradation that can lead to rapid changes in ice-rich permafrost landscapes. The process and its resulting landforms such as thermo-erosional gullies are reported to become increasingly active and widespread. (Re-)Activation of thermal erosion impacts the hydrological regime of affected landscapes and alters the biogeochemical composition of associated surface waters. Our study aims at assessing current rates and mechanisms of thermal erosion in small ice-rich permafrost catchments of Arctic Siberia. We investigated thermoerosional features in three different areas in and around the Lena River Delta that represent differing geomorphological, lithological and geocryological settings. We used a combination of field measurements, remote sensing methods including tacheometry, DGPS, and UAV surveys and subsequent GIS analyses to 1) quantify the morphometry of thermo-erosional landforms, 2) quantify the spatial extent of current thermo-erosional activity, and 3) quantify areal changes in activation and stabilization of thermal erosion over recent years to decades. Further data on snow depth and distribution in the gullies and valleys as well as hydrological and hydrochemical data of the associated streams aided the interpretation of observed spatial differences in thermal erosion rates and the development of active versus stabilized zones as well as their impacts on headwaters. Conference Object Arctic Arctic Ice lena river permafrost Siberia Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) Arctic
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 Thermal erosion is a prominent type of permafrost degradation that can lead to rapid changes in ice-rich permafrost landscapes. The process and its resulting landforms such as thermo-erosional gullies are reported to become increasingly active and widespread. (Re-)Activation of thermal erosion impacts the hydrological regime of affected landscapes and alters the biogeochemical composition of associated surface waters. Our study aims at assessing current rates and mechanisms of thermal erosion in small ice-rich permafrost catchments of Arctic Siberia. We investigated thermoerosional features in three different areas in and around the Lena River Delta that represent differing geomorphological, lithological and geocryological settings. We used a combination of field measurements, remote sensing methods including tacheometry, DGPS, and UAV surveys and subsequent GIS analyses to 1) quantify the morphometry of thermo-erosional landforms, 2) quantify the spatial extent of current thermo-erosional activity, and 3) quantify areal changes in activation and stabilization of thermal erosion over recent years to decades. Further data on snow depth and distribution in the gullies and valleys as well as hydrological and hydrochemical data of the associated streams aided the interpretation of observed spatial differences in thermal erosion rates and the development of active versus stabilized zones as well as their impacts on headwaters.
format Conference Object
author Morgenstern, Anne
Tarbeeva, Anna
Lebedeva, Lyudmila
Shamov, Vladimir
Inauen, Cornelia
spellingShingle Morgenstern, Anne
Tarbeeva, Anna
Lebedeva, Lyudmila
Shamov, Vladimir
Inauen, Cornelia
Characteristics and recent dynamics of thermo-erosional features in small catchments of Arctic Siberia
author_facet Morgenstern, Anne
Tarbeeva, Anna
Lebedeva, Lyudmila
Shamov, Vladimir
Inauen, Cornelia
author_sort Morgenstern, Anne
title Characteristics and recent dynamics of thermo-erosional features in small catchments of Arctic Siberia
title_short Characteristics and recent dynamics of thermo-erosional features in small catchments of Arctic Siberia
title_full Characteristics and recent dynamics of thermo-erosional features in small catchments of Arctic Siberia
title_fullStr Characteristics and recent dynamics of thermo-erosional features in small catchments of Arctic Siberia
title_full_unstemmed Characteristics and recent dynamics of thermo-erosional features in small catchments of Arctic Siberia
title_sort characteristics and recent dynamics of thermo-erosional features in small catchments of arctic siberia
publishDate 2023
url https://epic.awi.de/id/eprint/57841/
https://epic.awi.de/id/eprint/57841/1/EUCOP2023-ABSTRACTS_Morgenstern.pdf
https://hdl.handle.net/10013/epic.51798c3f-8d47-4553-8d5b-572260362444
geographic Arctic
geographic_facet Arctic
genre Arctic
Arctic
Ice
lena river
permafrost
Siberia
genre_facet Arctic
Arctic
Ice
lena river
permafrost
Siberia
op_source EPIC3
op_relation https://epic.awi.de/id/eprint/57841/1/EUCOP2023-ABSTRACTS_Morgenstern.pdf
Morgenstern, A. orcid:0000-0002-6466-7571 , Tarbeeva, A. , Lebedeva, L. , Shamov, V. and Inauen, C. (2023) Characteristics and recent dynamics of thermo-erosional features in small catchments of Arctic Siberia hdl:10013/epic.51798c3f-8d47-4553-8d5b-572260362444
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