Permafrost affected large rivers bed morphology: “Holes” in the bed of Kolyma river

The increase of water and sediment runoff in the Arctic significantly impacts the contemporary morphology of polar river channels fingerprinting climate change. This study focuses on the behaviour of non-cohesive riverbed sediments in the estuary section of the great Arctic river. We conducted a fie...

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Main Authors: Habel, M., Sergey, C., Victor, I., Vasily, E., Damian, C., Koffi, B.
Format: Conference Object
Language:English
Published: 2023
Subjects:
Online Access:https://gfzpublic.gfz-potsdam.de/pubman/item/item_5019308
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spelling ftgfzpotsdam:oai:gfzpublic.gfz-potsdam.de:item_5019308 2023-09-05T13:17:06+02:00 Permafrost affected large rivers bed morphology: “Holes” in the bed of Kolyma river Habel, M. Sergey, C. Victor, I. Vasily, E. Damian, C. Koffi, B. 2023 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5019308 eng eng info:eu-repo/semantics/altIdentifier/doi/10.57757/IUGG23-2607 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5019308 XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG) info:eu-repo/semantics/conferenceObject 2023 ftgfzpotsdam https://doi.org/10.57757/IUGG23-2607 2023-08-13T23:41:23Z The increase of water and sediment runoff in the Arctic significantly impacts the contemporary morphology of polar river channels fingerprinting climate change. This study focuses on the behaviour of non-cohesive riverbed sediments in the estuary section of the great Arctic river. We conducted a field study in the Kolyma River (Saha-Yakutia) and identified specific bed forms which form "holes" with similar depths of up to 25 - 27 m, with steep slopes with an inclination of 50° to 85°. Using field data and extended bathymetry maps, we created, calibrated and validated a high-resolute 2D morphological model. A few simulation scenarios for estimating bedform dimensions are examined to assess the ability to predict bedform parameters (length and depth) in a non-cohesive bed river. The relationship between bedform geometry (depth and the length of bedforms) and flow parameters, including shear velocity, and transport stage parameters, is investigated. The study was conducted under Trans-National Access from the European Union’s Horizon 2020 project INTERACT, under grant agreement No 730938, acronym: KolymaSed, title: “Assessment of sediment fluxes in the lower Kolyma River System, Siberia, Russia” Conference Object Arctic Climate change kolyma river permafrost Yakutia Siberia GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam) Arctic Kolyma ENVELOPE(161.000,161.000,69.500,69.500)
institution Open Polar
collection GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam)
op_collection_id ftgfzpotsdam
language English
description The increase of water and sediment runoff in the Arctic significantly impacts the contemporary morphology of polar river channels fingerprinting climate change. This study focuses on the behaviour of non-cohesive riverbed sediments in the estuary section of the great Arctic river. We conducted a field study in the Kolyma River (Saha-Yakutia) and identified specific bed forms which form "holes" with similar depths of up to 25 - 27 m, with steep slopes with an inclination of 50° to 85°. Using field data and extended bathymetry maps, we created, calibrated and validated a high-resolute 2D morphological model. A few simulation scenarios for estimating bedform dimensions are examined to assess the ability to predict bedform parameters (length and depth) in a non-cohesive bed river. The relationship between bedform geometry (depth and the length of bedforms) and flow parameters, including shear velocity, and transport stage parameters, is investigated. The study was conducted under Trans-National Access from the European Union’s Horizon 2020 project INTERACT, under grant agreement No 730938, acronym: KolymaSed, title: “Assessment of sediment fluxes in the lower Kolyma River System, Siberia, Russia”
format Conference Object
author Habel, M.
Sergey, C.
Victor, I.
Vasily, E.
Damian, C.
Koffi, B.
spellingShingle Habel, M.
Sergey, C.
Victor, I.
Vasily, E.
Damian, C.
Koffi, B.
Permafrost affected large rivers bed morphology: “Holes” in the bed of Kolyma river
author_facet Habel, M.
Sergey, C.
Victor, I.
Vasily, E.
Damian, C.
Koffi, B.
author_sort Habel, M.
title Permafrost affected large rivers bed morphology: “Holes” in the bed of Kolyma river
title_short Permafrost affected large rivers bed morphology: “Holes” in the bed of Kolyma river
title_full Permafrost affected large rivers bed morphology: “Holes” in the bed of Kolyma river
title_fullStr Permafrost affected large rivers bed morphology: “Holes” in the bed of Kolyma river
title_full_unstemmed Permafrost affected large rivers bed morphology: “Holes” in the bed of Kolyma river
title_sort permafrost affected large rivers bed morphology: “holes” in the bed of kolyma river
publishDate 2023
url https://gfzpublic.gfz-potsdam.de/pubman/item/item_5019308
long_lat ENVELOPE(161.000,161.000,69.500,69.500)
geographic Arctic
Kolyma
geographic_facet Arctic
Kolyma
genre Arctic
Climate change
kolyma river
permafrost
Yakutia
Siberia
genre_facet Arctic
Climate change
kolyma river
permafrost
Yakutia
Siberia
op_source XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG)
op_relation info:eu-repo/semantics/altIdentifier/doi/10.57757/IUGG23-2607
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5019308
op_doi https://doi.org/10.57757/IUGG23-2607
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