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СОВРЕМЕННЫЕ ПРОБЛЕМЫ СОСТОЯНИЯ РЕК КРИОЛИТОЗОНЫ

EFFECT OF SPEED DISTRIBUTION AT THE TURN OF THE CHANNEL ON EROSION

MATHEMATICAL RAINFALL MODEL FOR HYDROGRAPHIC DEMARCATION OF MANABI (ECUADOR)

INFLUENCE OF FLOW ON THAWING OF UNDERWATER SLOPES AND THE PACE COASTAL EROSION OF RIVERS, OCCURRING IN THE PERMAFROST ZONE

LABORATORY STUDY OF MOVEMENT OF RIVER IN THE PERMAFROST ON THE CHANNEL TURN

THE DEPENDENCE OF DESTRUCTIVE PROCESSES IN THE RIVERBED, INCLUDING IN THE TURN, FROM THE NUMBER OF REYNOLDS

The Seasonal Deformations of the Coastal Slopes in the Permafrost Zone

LABORATORY STUDIES EQUILIBRIUM PROFILE BANK OF THE RESERVOIR UNDER SIMULATED INTRAPERMAFROST

Erosion processes in section of channel bend in cryolithozone

Strength of frozen soils during thawing

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