Distribution of Glaze-Rime Deposits in the Lower 300-Meter Layer of the Atmosphere
Ice glaze-rime deposits produce very sizeable loads on structures. Intense deposits cause breaks in wire and power transmission lines (PTL) and communication lines (CL), collapsing of supports, demolition of towers, antennas, and so on. Therefore in designing and operating PTL, CL, and various kinds...
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ftdtic:AD0785965 2023-05-15T16:37:21+02:00 Distribution of Glaze-Rime Deposits in the Lower 300-Meter Layer of the Atmosphere Glukhov,V. G. ARMY FOREIGN SCIENCE AND TECHNOLOGY CENTER CHARLOTTESVILLE VA 1974-03-18 text/html http://www.dtic.mil/docs/citations/AD0785965 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0785965 en eng http://www.dtic.mil/docs/citations/AD0785965 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Snow Ice and Permafrost Electrical and Electronic Equipment *Ice formation *Transmission lines Translations USSR *Power lines Text 1974 ftdtic 2016-02-19T04:43:23Z Ice glaze-rime deposits produce very sizeable loads on structures. Intense deposits cause breaks in wire and power transmission lines (PTL) and communication lines (CL), collapsing of supports, demolition of towers, antennas, and so on. Therefore in designing and operating PTL, CL, and various kinds of tall structures, one must know the possible load they must bear of glaze and rime. From observations on Obnisk Tower in the winter of 1963-1964 a detailed study was made of several cases of glaze and rime formation in the moist near-cloud layer, fog, and in radiation cooling. The aim of this study is to generalize from observational data made of glaze in the 300 m layer, taken at the Obnisk Tower in 1962-1967. Unedited trans. of Glavnaya Geofizicheskaya Observatoriya, Leningrad. Trudy (USSR) n246 p63-72 n.d. Text Ice permafrost Defense Technical Information Center: DTIC Technical Reports database Rime ENVELOPE(6.483,6.483,62.567,62.567) |
institution |
Open Polar |
collection |
Defense Technical Information Center: DTIC Technical Reports database |
op_collection_id |
ftdtic |
language |
English |
topic |
Snow Ice and Permafrost Electrical and Electronic Equipment *Ice formation *Transmission lines Translations USSR *Power lines |
spellingShingle |
Snow Ice and Permafrost Electrical and Electronic Equipment *Ice formation *Transmission lines Translations USSR *Power lines Glukhov,V. G. Distribution of Glaze-Rime Deposits in the Lower 300-Meter Layer of the Atmosphere |
topic_facet |
Snow Ice and Permafrost Electrical and Electronic Equipment *Ice formation *Transmission lines Translations USSR *Power lines |
description |
Ice glaze-rime deposits produce very sizeable loads on structures. Intense deposits cause breaks in wire and power transmission lines (PTL) and communication lines (CL), collapsing of supports, demolition of towers, antennas, and so on. Therefore in designing and operating PTL, CL, and various kinds of tall structures, one must know the possible load they must bear of glaze and rime. From observations on Obnisk Tower in the winter of 1963-1964 a detailed study was made of several cases of glaze and rime formation in the moist near-cloud layer, fog, and in radiation cooling. The aim of this study is to generalize from observational data made of glaze in the 300 m layer, taken at the Obnisk Tower in 1962-1967. Unedited trans. of Glavnaya Geofizicheskaya Observatoriya, Leningrad. Trudy (USSR) n246 p63-72 n.d. |
author2 |
ARMY FOREIGN SCIENCE AND TECHNOLOGY CENTER CHARLOTTESVILLE VA |
format |
Text |
author |
Glukhov,V. G. |
author_facet |
Glukhov,V. G. |
author_sort |
Glukhov,V. G. |
title |
Distribution of Glaze-Rime Deposits in the Lower 300-Meter Layer of the Atmosphere |
title_short |
Distribution of Glaze-Rime Deposits in the Lower 300-Meter Layer of the Atmosphere |
title_full |
Distribution of Glaze-Rime Deposits in the Lower 300-Meter Layer of the Atmosphere |
title_fullStr |
Distribution of Glaze-Rime Deposits in the Lower 300-Meter Layer of the Atmosphere |
title_full_unstemmed |
Distribution of Glaze-Rime Deposits in the Lower 300-Meter Layer of the Atmosphere |
title_sort |
distribution of glaze-rime deposits in the lower 300-meter layer of the atmosphere |
publishDate |
1974 |
url |
http://www.dtic.mil/docs/citations/AD0785965 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0785965 |
long_lat |
ENVELOPE(6.483,6.483,62.567,62.567) |
geographic |
Rime |
geographic_facet |
Rime |
genre |
Ice permafrost |
genre_facet |
Ice permafrost |
op_source |
DTIC AND NTIS |
op_relation |
http://www.dtic.mil/docs/citations/AD0785965 |
op_rights |
APPROVED FOR PUBLIC RELEASE |
_version_ |
1766027640956780544 |