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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Main Author: A.V. Chernov
Format: Article in Journal/Newspaper
Language:English
Published: Zenodo 2018
Subjects:
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