Ice Cover of the Sea of Azov (Ledyanoi Pokrov Azovskogo Morya)

The detailed study of the ice cover in the Sea of Azov is based on data obtained during two or three preceding decades which are, in addition, reevaluated in the light of the latest systematic observations. On the basis of the data, the average dates for the four major phases of ice conditions, name...

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Bibliographic Details
Main Author: Shustov,B. S.
Other Authors: NAVAL OCEANOGRAPHIC OFFICE WASHINGTON D C
Format: Text
Language:English
Published: 1964
Subjects:
Ice
Online Access:http://www.dtic.mil/docs/citations/AD0718173
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0718173
id ftdtic:AD0718173
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spelling ftdtic:AD0718173 2023-05-15T16:37:15+02:00 Ice Cover of the Sea of Azov (Ledyanoi Pokrov Azovskogo Morya) Shustov,B. S. NAVAL OCEANOGRAPHIC OFFICE WASHINGTON D C 1964 text/html http://www.dtic.mil/docs/citations/AD0718173 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0718173 en eng http://www.dtic.mil/docs/citations/AD0718173 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Physical and Dynamic Oceanography Snow Ice and Permafrost (*SEA ICE MEASUREMENT) FREEZING MELTING CRACKS PERIODIC VARIATIONS THICKNESS COOLING WIND COASTAL REGIONS NAVIGATION HARBORS WATER TRAFFIC ECONOMICS USSR AZOV SEA ICE COVER TRANSLATIONS Text 1964 ftdtic 2016-02-19T00:23:55Z The detailed study of the ice cover in the Sea of Azov is based on data obtained during two or three preceding decades which are, in addition, reevaluated in the light of the latest systematic observations. On the basis of the data, the average dates for the four major phases of ice conditions, namely the appearance, freeze-up, breakup, and disappearance of ice, in various locations of the sea have been calculated and tabulated. Also the frequency percentages of the phases by ten-day periods have been calculated. The dates and frequency percentages, including data on ice thickness, disclose that the degree of iciness is greater and its period is longer in areas enclosed by the continent, as for instance in Taganrog area, where the land mass and colder air facilitate the cooling of water and the formation of ice. Also the effect of prevailing winds and climatic characteristics in various sea and coastal areas is discussed. (Author) Trans. of Moscow Univ. Fiziko-Mekhanicheskii Matematicheskii Fakultet. Izvestiya (USSR) v3 n1A p103-127 1930, by M. Slessers. Also available as TT-64-19193. Text Ice permafrost Sea ice 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 Physical and Dynamic Oceanography
Snow
Ice and Permafrost
(*SEA ICE
MEASUREMENT)
FREEZING
MELTING
CRACKS
PERIODIC VARIATIONS
THICKNESS
COOLING
WIND
COASTAL REGIONS
NAVIGATION
HARBORS
WATER TRAFFIC
ECONOMICS
USSR
AZOV SEA
ICE COVER
TRANSLATIONS
spellingShingle Physical and Dynamic Oceanography
Snow
Ice and Permafrost
(*SEA ICE
MEASUREMENT)
FREEZING
MELTING
CRACKS
PERIODIC VARIATIONS
THICKNESS
COOLING
WIND
COASTAL REGIONS
NAVIGATION
HARBORS
WATER TRAFFIC
ECONOMICS
USSR
AZOV SEA
ICE COVER
TRANSLATIONS
Shustov,B. S.
Ice Cover of the Sea of Azov (Ledyanoi Pokrov Azovskogo Morya)
topic_facet Physical and Dynamic Oceanography
Snow
Ice and Permafrost
(*SEA ICE
MEASUREMENT)
FREEZING
MELTING
CRACKS
PERIODIC VARIATIONS
THICKNESS
COOLING
WIND
COASTAL REGIONS
NAVIGATION
HARBORS
WATER TRAFFIC
ECONOMICS
USSR
AZOV SEA
ICE COVER
TRANSLATIONS
description The detailed study of the ice cover in the Sea of Azov is based on data obtained during two or three preceding decades which are, in addition, reevaluated in the light of the latest systematic observations. On the basis of the data, the average dates for the four major phases of ice conditions, namely the appearance, freeze-up, breakup, and disappearance of ice, in various locations of the sea have been calculated and tabulated. Also the frequency percentages of the phases by ten-day periods have been calculated. The dates and frequency percentages, including data on ice thickness, disclose that the degree of iciness is greater and its period is longer in areas enclosed by the continent, as for instance in Taganrog area, where the land mass and colder air facilitate the cooling of water and the formation of ice. Also the effect of prevailing winds and climatic characteristics in various sea and coastal areas is discussed. (Author) Trans. of Moscow Univ. Fiziko-Mekhanicheskii Matematicheskii Fakultet. Izvestiya (USSR) v3 n1A p103-127 1930, by M. Slessers. Also available as TT-64-19193.
author2 NAVAL OCEANOGRAPHIC OFFICE WASHINGTON D C
format Text
author Shustov,B. S.
author_facet Shustov,B. S.
author_sort Shustov,B. S.
title Ice Cover of the Sea of Azov (Ledyanoi Pokrov Azovskogo Morya)
title_short Ice Cover of the Sea of Azov (Ledyanoi Pokrov Azovskogo Morya)
title_full Ice Cover of the Sea of Azov (Ledyanoi Pokrov Azovskogo Morya)
title_fullStr Ice Cover of the Sea of Azov (Ledyanoi Pokrov Azovskogo Morya)
title_full_unstemmed Ice Cover of the Sea of Azov (Ledyanoi Pokrov Azovskogo Morya)
title_sort ice cover of the sea of azov (ledyanoi pokrov azovskogo morya)
publishDate 1964
url http://www.dtic.mil/docs/citations/AD0718173
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0718173
genre Ice
permafrost
Sea ice
genre_facet Ice
permafrost
Sea ice
op_source DTIC AND NTIS
op_relation http://www.dtic.mil/docs/citations/AD0718173
op_rights APPROVED FOR PUBLIC RELEASE
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