Morphological features of river channels and floodplains in the Far East of Russia under various natural conditions
Geographical analysis of river channel processes in rivers located along the meridional transect, running from the Arctic Ocean coast to Tibet and the East China Sea, confirmed that fluvial processes dominate in the formation of morphology and dynamics of river channels and floodplains in all natura...
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Format: | Article in Journal/Newspaper |
Language: | English |
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Zenodo
2018
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Online Access: | https://doi.org/10.5281/zenodo.1314020 |
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author | A.V. Chernov |
author_facet | A.V. Chernov |
author_sort | A.V. Chernov |
collection | Zenodo |
description | Geographical analysis of river channel processes in rivers located along the meridional transect, running from the Arctic Ocean coast to Tibet and the East China Sea, confirmed that fluvial processes dominate in the formation of morphology and dynamics of river channels and floodplains in all natural zones and under different conditions of channel deformation development. However, even a small disturbance in “climate” conditions by other exogenous geomorphological processes changes the morphology and dynamics of channels and floodplains as well as the dynamics of fluvial processes. The effect of zonal factors depends on the size of a given river and is more pronounced in medium and small rivers than the large ones. Furthermore, the effect of zonal factors on the processes of river channels and floodplains depends on specific environmental conditions of the climate zones: the more extreme the manifestation of certain climatic phenomena, the more pronounced they are in the morphology and dynamics of river channels and floodplains. |
format | Article in Journal/Newspaper |
genre | Arctic Arctic Ocean |
genre_facet | Arctic Arctic Ocean |
geographic | Arctic Arctic Ocean |
geographic_facet | Arctic Arctic Ocean |
id | ftzenodo:oai:zenodo.org:1314020 |
institution | Open Polar |
language | English |
op_collection_id | ftzenodo |
op_doi | https://doi.org/10.5281/zenodo.131402010.5281/zenodo.1314019 |
op_relation | https://doi.org/10.5281/zenodo.1314019 https://doi.org/10.5281/zenodo.1314020 oai:zenodo.org:1314020 |
op_rights | info:eu-repo/semantics/openAccess Creative Commons Attribution Non Commercial 4.0 International https://creativecommons.org/licenses/by-nc/4.0/legalcode |
op_source | GEOGRAPHY AND TOURISM, 6(1), (2018-06-30) |
publishDate | 2018 |
publisher | Zenodo |
record_format | openpolar |
spelling | ftzenodo:oai:zenodo.org:1314020 2025-01-16T20:37:55+00:00 Morphological features of river channels and floodplains in the Far East of Russia under various natural conditions A.V. Chernov 2018-06-30 https://doi.org/10.5281/zenodo.1314020 eng eng Zenodo https://doi.org/10.5281/zenodo.1314019 https://doi.org/10.5281/zenodo.1314020 oai:zenodo.org:1314020 info:eu-repo/semantics/openAccess Creative Commons Attribution Non Commercial 4.0 International https://creativecommons.org/licenses/by-nc/4.0/legalcode GEOGRAPHY AND TOURISM, 6(1), (2018-06-30) riverbeds floodplains climatic factors of channel processes local factors of fluvial processes info:eu-repo/semantics/article 2018 ftzenodo https://doi.org/10.5281/zenodo.131402010.5281/zenodo.1314019 2024-12-06T05:33:17Z Geographical analysis of river channel processes in rivers located along the meridional transect, running from the Arctic Ocean coast to Tibet and the East China Sea, confirmed that fluvial processes dominate in the formation of morphology and dynamics of river channels and floodplains in all natural zones and under different conditions of channel deformation development. However, even a small disturbance in “climate” conditions by other exogenous geomorphological processes changes the morphology and dynamics of channels and floodplains as well as the dynamics of fluvial processes. The effect of zonal factors depends on the size of a given river and is more pronounced in medium and small rivers than the large ones. Furthermore, the effect of zonal factors on the processes of river channels and floodplains depends on specific environmental conditions of the climate zones: the more extreme the manifestation of certain climatic phenomena, the more pronounced they are in the morphology and dynamics of river channels and floodplains. Article in Journal/Newspaper Arctic Arctic Ocean Zenodo Arctic Arctic Ocean |
spellingShingle | riverbeds floodplains climatic factors of channel processes local factors of fluvial processes A.V. Chernov Morphological features of river channels and floodplains in the Far East of Russia under various natural conditions |
title | Morphological features of river channels and floodplains in the Far East of Russia under various natural conditions |
title_full | Morphological features of river channels and floodplains in the Far East of Russia under various natural conditions |
title_fullStr | Morphological features of river channels and floodplains in the Far East of Russia under various natural conditions |
title_full_unstemmed | Morphological features of river channels and floodplains in the Far East of Russia under various natural conditions |
title_short | Morphological features of river channels and floodplains in the Far East of Russia under various natural conditions |
title_sort | morphological features of river channels and floodplains in the far east of russia under various natural conditions |
topic | riverbeds floodplains climatic factors of channel processes local factors of fluvial processes |
topic_facet | riverbeds floodplains climatic factors of channel processes local factors of fluvial processes |
url | https://doi.org/10.5281/zenodo.1314020 |