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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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 |
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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 |
_version_ |
1766027547361935360 |