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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-covered flows in straight reaches of rivers are presented. Special attention is paid to modern studies of features of flow in a river bend.
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-covered flows in straight reaches of rivers are presented. Special attention is paid to modern studies of features of flow in a river bend.
Flow Structure in a River Bend in the Cryolithozone
Dolgopolova, E. N. (author)
2020
Article (Journal)
Electronic Resource
English
BKL:
56.30
Wasserbau
/
56.30$jWasserbau
Flow Structure in a River Bend in the Cryolithozone
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