Implications of Yedoma bank outcrops on the polar’s river sediment transport ...
<!--!introduction!--> The erosion of permafrost outcrops (yedoma) in the valleys of large Arctic rivers is considered as an important source of suspended sediment and carbon inflow into the natural waters of the Lena, Kolyma, Yana, Indigirka Rivers and further into the Arctic Ocean. Based on c...
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GFZ German Research Centre for Geosciences
2023
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Online Access: | https://dx.doi.org/10.57757/iugg23-2337 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5018420 |
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ftdatacite:10.57757/iugg23-2337 2023-07-23T04:17:33+02:00 Implications of Yedoma bank outcrops on the polar’s river sediment transport ... Chalov, Sergey Habel, Michał Moreido, Vsevolod Prokopeva, Kristina 2023 https://dx.doi.org/10.57757/iugg23-2337 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5018420 unknown GFZ German Research Centre for Geosciences Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 Article ConferencePaper Oral 2023 ftdatacite https://doi.org/10.57757/iugg23-2337 2023-07-03T17:56:50Z <!--!introduction!--> The erosion of permafrost outcrops (yedoma) in the valleys of large Arctic rivers is considered as an important source of suspended sediment and carbon inflow into the natural waters of the Lena, Kolyma, Yana, Indigirka Rivers and further into the Arctic Ocean. Based on combination of on-situ sediment transport observations done in 2021 and 2022 (reconnaissance, ADCP measurements, laser optics LISST profiles), application of remote sensing data and 2D hydrodynamic and morphological modelling by MIKE 21C, we explored the impact of Duvanny Yar Yedoma ice complex, the largest inland outcrop of permafrost, on lower reaches of the Kolyma river. An increase of around 20% in the turbidity of the Kolyma River was revealed during the summer low-flows in the reach downstream of the yedoma. The influx of suspended matter due to the melting of the slopes of the ice complex on hot summer days in the emerging network of turbidity streams was estimated at a value of more than 5 kg/s. The effect ... : The 28th IUGG General Assembly (IUGG2023) (Berlin 2023) ... Conference Object Arctic Arctic Ocean Ice kolyma river permafrost DataCite Metadata Store (German National Library of Science and Technology) Arctic Arctic Ocean Kolyma ENVELOPE(161.000,161.000,69.500,69.500) Indigirka ENVELOPE(149.609,149.609,70.929,70.929) Yar ENVELOPE(151.300,151.300,70.917,70.917) |
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Open Polar |
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DataCite Metadata Store (German National Library of Science and Technology) |
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<!--!introduction!--> The erosion of permafrost outcrops (yedoma) in the valleys of large Arctic rivers is considered as an important source of suspended sediment and carbon inflow into the natural waters of the Lena, Kolyma, Yana, Indigirka Rivers and further into the Arctic Ocean. Based on combination of on-situ sediment transport observations done in 2021 and 2022 (reconnaissance, ADCP measurements, laser optics LISST profiles), application of remote sensing data and 2D hydrodynamic and morphological modelling by MIKE 21C, we explored the impact of Duvanny Yar Yedoma ice complex, the largest inland outcrop of permafrost, on lower reaches of the Kolyma river. An increase of around 20% in the turbidity of the Kolyma River was revealed during the summer low-flows in the reach downstream of the yedoma. The influx of suspended matter due to the melting of the slopes of the ice complex on hot summer days in the emerging network of turbidity streams was estimated at a value of more than 5 kg/s. The effect ... : The 28th IUGG General Assembly (IUGG2023) (Berlin 2023) ... |
format |
Conference Object |
author |
Chalov, Sergey Habel, Michał Moreido, Vsevolod Prokopeva, Kristina |
spellingShingle |
Chalov, Sergey Habel, Michał Moreido, Vsevolod Prokopeva, Kristina Implications of Yedoma bank outcrops on the polar’s river sediment transport ... |
author_facet |
Chalov, Sergey Habel, Michał Moreido, Vsevolod Prokopeva, Kristina |
author_sort |
Chalov, Sergey |
title |
Implications of Yedoma bank outcrops on the polar’s river sediment transport ... |
title_short |
Implications of Yedoma bank outcrops on the polar’s river sediment transport ... |
title_full |
Implications of Yedoma bank outcrops on the polar’s river sediment transport ... |
title_fullStr |
Implications of Yedoma bank outcrops on the polar’s river sediment transport ... |
title_full_unstemmed |
Implications of Yedoma bank outcrops on the polar’s river sediment transport ... |
title_sort |
implications of yedoma bank outcrops on the polar’s river sediment transport ... |
publisher |
GFZ German Research Centre for Geosciences |
publishDate |
2023 |
url |
https://dx.doi.org/10.57757/iugg23-2337 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5018420 |
long_lat |
ENVELOPE(161.000,161.000,69.500,69.500) ENVELOPE(149.609,149.609,70.929,70.929) ENVELOPE(151.300,151.300,70.917,70.917) |
geographic |
Arctic Arctic Ocean Kolyma Indigirka Yar |
geographic_facet |
Arctic Arctic Ocean Kolyma Indigirka Yar |
genre |
Arctic Arctic Ocean Ice kolyma river permafrost |
genre_facet |
Arctic Arctic Ocean Ice kolyma river permafrost |
op_rights |
Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 |
op_doi |
https://doi.org/10.57757/iugg23-2337 |
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1772179411353731072 |