Characteristics of the Formation of River Slope Run-off in Permafrost Regions (Osobennosti Formirovaniia Sklonovogo Stoka Rek Zony Mnogoletnei Merzloty)

This report discusses questions concerning the formation of a slope runoff in the case of a deep lie of the permafrost water confining layer and available length slope thickness of the thaw layer. It is under such conditions that most floods form in mountainous rivers of the northeatern USSR. (Autho...

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Bibliographic Details
Main Author: Gopchenko,E D
Other Authors: COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER N H
Format: Text
Language:English
Published: 1978
Subjects:
Hydrology
Limnology and Potamology
Snow
Ice and Permafrost
*RUNOFF
*PERMAFROST
MATHEMATICAL MODELS
USSR
SLOPE
TRANSLATIONS
RIVERS
WATER EROSION
Ice
permafrost
Online Access:http://www.dtic.mil/docs/citations/ADA053226
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA053226
Description
Summary:This report discusses questions concerning the formation of a slope runoff in the case of a deep lie of the permafrost water confining layer and available length slope thickness of the thaw layer. It is under such conditions that most floods form in mountainous rivers of the northeatern USSR. (Author) Trans. of Meteorologiia, Klimatologiia i Gidrologiia (USSR) v10 p140-144, 1974.

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