DETERMINING THE THICKNESS OF MOUNTAIN GLACIERS BY THE 'BALANCES METHOD'

The balances method depends on the following data: in the highest degree on the precision of the data employed: on the following data: the ablation data, the surface levels survey, the morphometry of the glacier, and the speed of its movement. Trans. of Vsesoyuznee Geograficheskee Obshchestve. Izves...

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Bibliographic Details
Main Author: Palgov,N. N.
Other Authors: DIRECTORATE OF SCIENTIFIC INFORMATION SERVICES OTTAWA (ONTARIO)
Format: Text
Language:English
Published: 1965
Subjects:
Snow
Ice and Permafrost
(*GLACIERS
MEASUREMENT)
ICE
THICKNESS
DETERMINATION
USSR
Ice
permafrost
Online Access:http://www.dtic.mil/docs/citations/AD0626445
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0626445
Description
Summary:The balances method depends on the following data: in the highest degree on the precision of the data employed: on the following data: the ablation data, the surface levels survey, the morphometry of the glacier, and the speed of its movement. Trans. of Vsesoyuznee Geograficheskee Obshchestve. Izvestiya (USSR) v90 p170-6 1958. Also available from NRC as C-5467.

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