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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ftdtic:AD0626445 2023-05-15T16:37:01+02:00 DETERMINING THE THICKNESS OF MOUNTAIN GLACIERS BY THE 'BALANCES METHOD' Palgov,N. N. DIRECTORATE OF SCIENTIFIC INFORMATION SERVICES OTTAWA (ONTARIO) 1965-06 text/html http://www.dtic.mil/docs/citations/AD0626445 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0626445 en eng http://www.dtic.mil/docs/citations/AD0626445 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Snow Ice and Permafrost (*GLACIERS MEASUREMENT) ICE THICKNESS DETERMINATION USSR Text 1965 ftdtic 2016-02-18T18:55:46Z 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. Text Ice permafrost Defense Technical Information Center: DTIC Technical Reports database |
institution |
Open Polar |
collection |
Defense Technical Information Center: DTIC Technical Reports database |
op_collection_id |
ftdtic |
language |
English |
topic |
Snow Ice and Permafrost (*GLACIERS MEASUREMENT) ICE THICKNESS DETERMINATION USSR |
spellingShingle |
Snow Ice and Permafrost (*GLACIERS MEASUREMENT) ICE THICKNESS DETERMINATION USSR Palgov,N. N. DETERMINING THE THICKNESS OF MOUNTAIN GLACIERS BY THE 'BALANCES METHOD' |
topic_facet |
Snow Ice and Permafrost (*GLACIERS MEASUREMENT) ICE THICKNESS DETERMINATION USSR |
description |
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. |
author2 |
DIRECTORATE OF SCIENTIFIC INFORMATION SERVICES OTTAWA (ONTARIO) |
format |
Text |
author |
Palgov,N. N. |
author_facet |
Palgov,N. N. |
author_sort |
Palgov,N. N. |
title |
DETERMINING THE THICKNESS OF MOUNTAIN GLACIERS BY THE 'BALANCES METHOD' |
title_short |
DETERMINING THE THICKNESS OF MOUNTAIN GLACIERS BY THE 'BALANCES METHOD' |
title_full |
DETERMINING THE THICKNESS OF MOUNTAIN GLACIERS BY THE 'BALANCES METHOD' |
title_fullStr |
DETERMINING THE THICKNESS OF MOUNTAIN GLACIERS BY THE 'BALANCES METHOD' |
title_full_unstemmed |
DETERMINING THE THICKNESS OF MOUNTAIN GLACIERS BY THE 'BALANCES METHOD' |
title_sort |
determining the thickness of mountain glaciers by the 'balances method' |
publishDate |
1965 |
url |
http://www.dtic.mil/docs/citations/AD0626445 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0626445 |
genre |
Ice permafrost |
genre_facet |
Ice permafrost |
op_source |
DTIC AND NTIS |
op_relation |
http://www.dtic.mil/docs/citations/AD0626445 |
op_rights |
APPROVED FOR PUBLIC RELEASE |
_version_ |
1766027322655244288 |