Islands of the upper River Ob: morphometric characteristic, evolution and dynamics

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Abstract

The studied reach of the upper River Ob is quite complicated in the morphological aspect and characterized by very low channel stability and high discharge of sand load. Unconstrained conditions for lateral channel migration promotes active channel deformations not only at long-term scale, but also seasonally. Channel deformations contribute to the transformation of the channel and its morphodynamic type in time. The upper River Ob is intensively used as a water course, so any reorganization of the channel and river islands should be taken into account to support navigation.

Morphometric and morphodynamic analysis of the islands made it possible to develop their morphological classification. Morphometric parameters of islands, being associated with the characteristics of the channel itself, are one of the main classification features. Empirical relations were obtained that link the dimensions (Lo, Bo) and shape of islands (Lo/Bo) with the morphodynamic channel type and its stability, the degree of branching of the channel (number of islands no per 1 km of channel length x). The features of island dynamics are also determined by the morphodynamic type of the channel and are associated with the morphometric characteristics of the islands themselves and their position in the channel, which determines the transgressive, regressive and transverse shift or their stable position in time.

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About the authors

G. B. Golubtsov

Lomonosov Moscow State University, Faculty of Geography

Author for correspondence.
Email: georgy1995golubcov@yandex.ru
Russian Federation, 1, Leninskie gory, Moscow, 119991

R. S. Chalov

Lomonosov Moscow State University, Faculty of Geography

Email: rschalov@mail.ru
Russian Federation, 1, Leninskie gory, Moscow, 119991

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Supplementary files

Supplementary Files
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1. JATS XML
2. Fig. 1. Dependence of the degree of branching of the channel of the upper Ob no / x on its stability (the coefficient of stability of the channel NI Makkaveeva Ks)

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3. Fig. 2. Fominsky – Ust-Anuysky knot of parallel-sleeve branching of the upper Ob

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4. Fig. 3. The ratio of the linear dimensions of the islands (Lo and Bo) for different types of branching: 1 - parallel-sleeve; 2 - one-sided and delta

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5. Fig. 4. Transgressive displacement of an elementary island in a parallel-sleeve channel of the upper Ob (satellite images: (a) - 2010, (b) - 2015 https://www.arcgis.com)

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6. Fig. 5. Island arrays of the Karpov one-sided branching of the upper Ob (space image, https://www.arcgis.com)

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