Flow Structure in a River Bend in the Cryolithozone

Rivers of the cryolithozone are under consideration. The structure of open-water and ice-covered flows in this zone is determined by moderate river falls, high sinuosity of rivers, especially delta branches, and long freeze up periods. The basic relationships describing the open-water and ice-covere...

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Bibliographic Details
Published in:Power technology and engineering 2020, Vol.54 (3), p.309-312
Main Author: Dolgopolova, E. N.
Format: Article
Language:English
Subjects:
Electrical Machines and Networks
Energy
Energy Systems
Foundations
Geoengineering
Hydraulics
Ice cover
Power Electronics
Renewable and Green Energy
Rivers
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Summary:Rivers of the cryolithozone are under consideration. The structure of open-water and ice-covered flows in this zone is determined by moderate river falls, high sinuosity of rivers, especially delta branches, and long freeze up periods. The basic relationships describing the open-water and ice-covered flows in straight reaches of rivers are presented. Special attention is paid to modern studies of features of flow in a river bend.
ISSN:1570-145X
1570-1468
DOI:10.1007/s10749-020-01207-w