Assessing sediment transfer in a large Arctic catchment using distributed runoff and soil erosion modelling

With global warming expected to be more pronounced in the Arctic regions, soil erosion and associated sediment input to river systems is subsequently subject to increase here, too. This study attempts to understand complex processes involved in runoff generation, and sediment transport in the Lena R...

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Main Authors: Moreido, V., Bugaets, A., Motovilov, Y., Chalov, S., Fingert, E.
Format: Conference Object
Language:English
Published: 2023
Subjects:
Online Access:https://gfzpublic.gfz-potsdam.de/pubman/item/item_5021481
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spelling ftgfzpotsdam:oai:gfzpublic.gfz-potsdam.de:item_5021481 2023-07-30T04:01:27+02:00 Assessing sediment transfer in a large Arctic catchment using distributed runoff and soil erosion modelling Moreido, V. Bugaets, A. Motovilov, Y. Chalov, S. Fingert, E. 2023-07-11 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5021481 eng eng info:eu-repo/semantics/altIdentifier/doi/10.57757/IUGG23-4041 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5021481 XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG) info:eu-repo/semantics/conferenceObject 2023 ftgfzpotsdam https://doi.org/10.57757/IUGG23-4041 2023-07-09T23:40:20Z With global warming expected to be more pronounced in the Arctic regions, soil erosion and associated sediment input to river systems is subsequently subject to increase here, too. This study attempts to understand complex processes involved in runoff generation, and sediment transport in the Lena River basin, and to quantify their respective fluxes at the river outlet. To assess the rate of soil erosion in the Lena River basin we augmented the regional distributed hydrological model ECOMAG with a soil erosion calculation routine MUSLE model. The ECOMAG model is used to generate runoff from a distributed network of elementary catchments, each having a unique distribution of hydrological response units accounting for various soil, vegetation and groundwater properties, as well as seasonal thawing of permafrost. For each elementary catchment the MUSLE routine was calculated on a daily timestep to assess the amount of sediment entering the stream network during snowmelt and rainfall. The model was calibrated using the available measurement data of streamflow and sediment runoff from the river gauging network. The selected approach allowed for correct simulation of the observed streamflow discharge and sediment load time-series and is applicable for the impact studies in this region. The study was conducted under RSF project 21-17-00181. Conference Object Arctic Global warming lena river permafrost GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam) Arctic
institution Open Polar
collection GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam)
op_collection_id ftgfzpotsdam
language English
description With global warming expected to be more pronounced in the Arctic regions, soil erosion and associated sediment input to river systems is subsequently subject to increase here, too. This study attempts to understand complex processes involved in runoff generation, and sediment transport in the Lena River basin, and to quantify their respective fluxes at the river outlet. To assess the rate of soil erosion in the Lena River basin we augmented the regional distributed hydrological model ECOMAG with a soil erosion calculation routine MUSLE model. The ECOMAG model is used to generate runoff from a distributed network of elementary catchments, each having a unique distribution of hydrological response units accounting for various soil, vegetation and groundwater properties, as well as seasonal thawing of permafrost. For each elementary catchment the MUSLE routine was calculated on a daily timestep to assess the amount of sediment entering the stream network during snowmelt and rainfall. The model was calibrated using the available measurement data of streamflow and sediment runoff from the river gauging network. The selected approach allowed for correct simulation of the observed streamflow discharge and sediment load time-series and is applicable for the impact studies in this region. The study was conducted under RSF project 21-17-00181.
format Conference Object
author Moreido, V.
Bugaets, A.
Motovilov, Y.
Chalov, S.
Fingert, E.
spellingShingle Moreido, V.
Bugaets, A.
Motovilov, Y.
Chalov, S.
Fingert, E.
Assessing sediment transfer in a large Arctic catchment using distributed runoff and soil erosion modelling
author_facet Moreido, V.
Bugaets, A.
Motovilov, Y.
Chalov, S.
Fingert, E.
author_sort Moreido, V.
title Assessing sediment transfer in a large Arctic catchment using distributed runoff and soil erosion modelling
title_short Assessing sediment transfer in a large Arctic catchment using distributed runoff and soil erosion modelling
title_full Assessing sediment transfer in a large Arctic catchment using distributed runoff and soil erosion modelling
title_fullStr Assessing sediment transfer in a large Arctic catchment using distributed runoff and soil erosion modelling
title_full_unstemmed Assessing sediment transfer in a large Arctic catchment using distributed runoff and soil erosion modelling
title_sort assessing sediment transfer in a large arctic catchment using distributed runoff and soil erosion modelling
publishDate 2023
url https://gfzpublic.gfz-potsdam.de/pubman/item/item_5021481
geographic Arctic
geographic_facet Arctic
genre Arctic
Global warming
lena river
permafrost
genre_facet Arctic
Global warming
lena river
permafrost
op_source XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG)
op_relation info:eu-repo/semantics/altIdentifier/doi/10.57757/IUGG23-4041
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5021481
op_doi https://doi.org/10.57757/IUGG23-4041
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