Landscape Reading for Alpine Rivers: A Case Study from the river Biya

Anthropogenic stressors have altered the hydromorphological characteristics of rivers worldwide. Environmental guiding principles are essential for planning sustainable river restoration measures. The alpine river Biya, located in the Russian Altai mountains, originates from Lake Teletskoye and join...

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Main Authors: Lisa Schmalfuß, Christoph Hauer, Liubov V. Yanygina, Martin Schletterer
Format: Article
Language:English
Published: Lomonosov Moscow State University 2023-01-01
Series:Geography, Environment, Sustainability
Subjects:
Online Access:https://ges.rgo.ru/jour/article/view/2736
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author Lisa Schmalfuß
Christoph Hauer
Liubov V. Yanygina
Martin Schletterer
author_facet Lisa Schmalfuß
Christoph Hauer
Liubov V. Yanygina
Martin Schletterer
author_sort Lisa Schmalfuß
collection DOAJ
description Anthropogenic stressors have altered the hydromorphological characteristics of rivers worldwide. Environmental guiding principles are essential for planning sustainable river restoration measures. The alpine river Biya, located in the Russian Altai mountains, originates from Lake Teletskoye and joins the Katun near Biysk, forming the Ob. The Biya represents a hydromorphological reference system in anthropogenically ‘least-disturbed’ condition. The presented study aimed to assess the river’s undisturbed morphology in relationship with the geological history of three different river stretches based on an adapted landscape reading approach using remote sensing information (ASTER GDEM v3). The established widths of the active channel, active floodplain and morphological floodplain as well as the longitudinal section were used to explain the differences between upper, middle, and lower Biya. The results confirm differences in the geological origins between the upper Biya, which has previously been described as the least developed and narrowest, and the other two stretches based on the analyses of morphological parameters. Morphological floodplain width could best explain the differences between upper (0-86 km), middle (86-196 km), and lower Biya (196-301 km). The study further showed a clear relationship between the variations in river patterns and adjacent topographic structures (valley confinements, tributary interactions), highlighting that any assessment of river morphology must consider the wider surroundings of a river stretch. The presented morphological observations and analyses of the Biya show that easily obtainable parameters can detect differences in the morphological history of river stretches within the same catchment, supporting process understanding.
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spelling doaj.art-db08a8bf89e14754a2ee52f4c8b35dd92024-10-17T12:30:11ZengLomonosov Moscow State UniversityGeography, Environment, Sustainability2071-93882542-15652023-01-0115419621310.24057/2071-9388-2022-046650Landscape Reading for Alpine Rivers: A Case Study from the river BiyaLisa Schmalfuß0Christoph Hauer1Liubov V. Yanygina2Martin Schletterer3Institute of Hydraulic Engineering and River Research, University of Natural Resources and Applied Life SciencesInstitute of Hydraulic Engineering and River Research, University of Natural Resources and Applied Life SciencesInstitute for Water and Environmental Problems SB RASInstitute of Hydrobiology and Aquatic Ecosystem Management, University of Natural Resources and Applied Life SciencesAnthropogenic stressors have altered the hydromorphological characteristics of rivers worldwide. Environmental guiding principles are essential for planning sustainable river restoration measures. The alpine river Biya, located in the Russian Altai mountains, originates from Lake Teletskoye and joins the Katun near Biysk, forming the Ob. The Biya represents a hydromorphological reference system in anthropogenically ‘least-disturbed’ condition. The presented study aimed to assess the river’s undisturbed morphology in relationship with the geological history of three different river stretches based on an adapted landscape reading approach using remote sensing information (ASTER GDEM v3). The established widths of the active channel, active floodplain and morphological floodplain as well as the longitudinal section were used to explain the differences between upper, middle, and lower Biya. The results confirm differences in the geological origins between the upper Biya, which has previously been described as the least developed and narrowest, and the other two stretches based on the analyses of morphological parameters. Morphological floodplain width could best explain the differences between upper (0-86 km), middle (86-196 km), and lower Biya (196-301 km). The study further showed a clear relationship between the variations in river patterns and adjacent topographic structures (valley confinements, tributary interactions), highlighting that any assessment of river morphology must consider the wider surroundings of a river stretch. The presented morphological observations and analyses of the Biya show that easily obtainable parameters can detect differences in the morphological history of river stretches within the same catchment, supporting process understanding.https://ges.rgo.ru/jour/article/view/2736hydromorphologyglacial historysinuositychannel evolutionremote sensing
spellingShingle Lisa Schmalfuß
Christoph Hauer
Liubov V. Yanygina
Martin Schletterer
Landscape Reading for Alpine Rivers: A Case Study from the river Biya
Geography, Environment, Sustainability
hydromorphology
glacial history
sinuosity
channel evolution
remote sensing
title Landscape Reading for Alpine Rivers: A Case Study from the river Biya
title_full Landscape Reading for Alpine Rivers: A Case Study from the river Biya
title_fullStr Landscape Reading for Alpine Rivers: A Case Study from the river Biya
title_full_unstemmed Landscape Reading for Alpine Rivers: A Case Study from the river Biya
title_short Landscape Reading for Alpine Rivers: A Case Study from the river Biya
title_sort landscape reading for alpine rivers a case study from the river biya
topic hydromorphology
glacial history
sinuosity
channel evolution
remote sensing
url https://ges.rgo.ru/jour/article/view/2736
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AT christophhauer landscapereadingforalpineriversacasestudyfromtheriverbiya
AT liubovvyanygina landscapereadingforalpineriversacasestudyfromtheriverbiya
AT martinschletterer landscapereadingforalpineriversacasestudyfromtheriverbiya