Dynamics of the River Channel Deformations along the Latitudinal Section of the Middle Reaches of the Ob River

The paper describes the dynamics of stream erosion of the right bank of the Ob river in the Nizhnevartovsk area in the Khanty-Mansi Autonomous Okrug – Yugra. Furthermore, it presents an analysis of fifteen-year monitoring of the river channel deformations at the Ust-Vakh observation station using fi...

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Main Author: S.E. Korkin
Format: Article in Journal/Newspaper
Language:English
Published: 2018
Subjects:
Online Access:https://zenodo.org/record/1314010
https://doi.org/10.5281/zenodo.1314010
id ftzenodo:oai:zenodo.org:1314010
record_format openpolar
spelling ftzenodo:oai:zenodo.org:1314010 2023-05-15T17:02:52+02:00 Dynamics of the River Channel Deformations along the Latitudinal Section of the Middle Reaches of the Ob River S.E. Korkin 2018-06-30 https://zenodo.org/record/1314010 https://doi.org/10.5281/zenodo.1314010 eng eng doi:10.5281/zenodo.1314009 https://zenodo.org/record/1314010 https://doi.org/10.5281/zenodo.1314010 oai:zenodo.org:1314010 info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by-nc/4.0/legalcode GEOGRAPHY AND TOURISM 6(1) river channel evolution river channel deformations riverbank range lateral erosion info:eu-repo/semantics/article publication-article 2018 ftzenodo https://doi.org/10.5281/zenodo.131401010.5281/zenodo.1314009 2023-03-10T18:38:45Z The paper describes the dynamics of stream erosion of the right bank of the Ob river in the Nizhnevartovsk area in the Khanty-Mansi Autonomous Okrug – Yugra. Furthermore, it presents an analysis of fifteen-year monitoring of the river channel deformations at the Ust-Vakh observation station using field-established benchmarks through interpretation of diachronous satellite images and registration of the riverbank line using the satellite positioning. The paper presents a comparison of methods and indicates their positive and negative aspects. The obtained survey results are required for the development of integrated engineering efforts to protect river banks at populated localities as part of the targeted program “Transfer of people from residential houses located in the floodplain zone exposed to erosion”. These surveys allow to accurately predict the dynamics of stream erosion of the river banks along the latitudinal section of the middle reaches of the Ob river, where various floodplain types are formed, banks are unprotected, islands occur in the river channel, and the floodplain is dissected by a braided river channel. Article in Journal/Newspaper khanty khanty-mansi ob river Mansi Zenodo
institution Open Polar
collection Zenodo
op_collection_id ftzenodo
language English
topic river channel evolution
river channel deformations
riverbank range
lateral erosion
spellingShingle river channel evolution
river channel deformations
riverbank range
lateral erosion
S.E. Korkin
Dynamics of the River Channel Deformations along the Latitudinal Section of the Middle Reaches of the Ob River
topic_facet river channel evolution
river channel deformations
riverbank range
lateral erosion
description The paper describes the dynamics of stream erosion of the right bank of the Ob river in the Nizhnevartovsk area in the Khanty-Mansi Autonomous Okrug – Yugra. Furthermore, it presents an analysis of fifteen-year monitoring of the river channel deformations at the Ust-Vakh observation station using field-established benchmarks through interpretation of diachronous satellite images and registration of the riverbank line using the satellite positioning. The paper presents a comparison of methods and indicates their positive and negative aspects. The obtained survey results are required for the development of integrated engineering efforts to protect river banks at populated localities as part of the targeted program “Transfer of people from residential houses located in the floodplain zone exposed to erosion”. These surveys allow to accurately predict the dynamics of stream erosion of the river banks along the latitudinal section of the middle reaches of the Ob river, where various floodplain types are formed, banks are unprotected, islands occur in the river channel, and the floodplain is dissected by a braided river channel.
format Article in Journal/Newspaper
author S.E. Korkin
author_facet S.E. Korkin
author_sort S.E. Korkin
title Dynamics of the River Channel Deformations along the Latitudinal Section of the Middle Reaches of the Ob River
title_short Dynamics of the River Channel Deformations along the Latitudinal Section of the Middle Reaches of the Ob River
title_full Dynamics of the River Channel Deformations along the Latitudinal Section of the Middle Reaches of the Ob River
title_fullStr Dynamics of the River Channel Deformations along the Latitudinal Section of the Middle Reaches of the Ob River
title_full_unstemmed Dynamics of the River Channel Deformations along the Latitudinal Section of the Middle Reaches of the Ob River
title_sort dynamics of the river channel deformations along the latitudinal section of the middle reaches of the ob river
publishDate 2018
url https://zenodo.org/record/1314010
https://doi.org/10.5281/zenodo.1314010
genre khanty
khanty-mansi
ob river
Mansi
genre_facet khanty
khanty-mansi
ob river
Mansi
op_source GEOGRAPHY AND TOURISM 6(1)
op_relation doi:10.5281/zenodo.1314009
https://zenodo.org/record/1314010
https://doi.org/10.5281/zenodo.1314010
oai:zenodo.org:1314010
op_rights info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by-nc/4.0/legalcode
op_doi https://doi.org/10.5281/zenodo.131401010.5281/zenodo.1314009
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