THE PROBABILITY AND INTENSITY OF ICING OF SEA-GOING VESSELS
VEROYATNOST' I INTENSIVNOST' OBLEDENENIYA MORSKIKH SUNDOV
Deals with ice formation on ships at sea and defines three rates of icing which occur on arctic seas. When the ship becomes covered with a thick ice layer, its center of gravity shifts upward and its stability in the water becomes doubtful. Slow icing takes place at recurrent negative temperatures in wind up to 9 m/sec. Rapid icing occurs with temperatures of -2 degrees C or less recurring and wind at greater than 10 m/sec, and icing becomes very rapid below -4 degrees C in wind below 10 m/sec. The distribution of these rates of icing is charted for the Okhotsk and Bering Seas and Gulf of Alaska.
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Corporate Authors:
Moskva, ni Insti Aeroklimatologii
Moscow, USSR -
Authors:
- Shekhtman, A N
- Publication Date: 1968
Language
- Russian
Media Info
- Features: References;
- Pagination: p. 55-65
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Serial:
- Issue Number: 50
Subject/Index Terms
- TRT Terms: Icing
- Old TRIS Terms: Icing processes
- Subject Areas: Hydraulics and Hydrology; Marine Transportation;
Filing Info
- Accession Number: 00037585
- Record Type: Publication
- Source Agency: Arctic Institute of North America
- Files: TRIS
- Created Date: Nov 10 1973 12:00AM