Drift Circulation in the Zone of the Subarctic Hydrological Front (O Dreifovoi Tsirkulyatsii v Zone Subpolyarnogo Gidrologicheskogo Fronta)

Calculation of drift circulation in the North Atlantic Ocean, from 40 to 65 degrees N, is discussed and evaluated. The speed and direction of drift currents is determined, and the effect of drift circulation on the seasonal position of front in surface water is specified. (Author) Trans. of Gosudars...

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Bibliographic Details
Main Author: Gruzinov,V. M.
Other Authors: NAVAL OCEANOGRAPHIC OFFICE WASHINGTON D C
Format: Text
Language:English
Published: 1969
Subjects:
Physical and Dynamic Oceanography
(*OCEAN CURRENTS
*ATLANTIC OCEAN)
DRIFT
VELOCITY
SURFACE PROPERTIES
WIND
PERIODIC VARIATIONS
DENSITY
USSR
NORTH ATLANTIC OCEAN
TRANSLATIONS
North Atlantic
Subarctic
Online Access:http://www.dtic.mil/docs/citations/AD0724269
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0724269
Description
Summary:Calculation of drift circulation in the North Atlantic Ocean, from 40 to 65 degrees N, is discussed and evaluated. The speed and direction of drift currents is determined, and the effect of drift circulation on the seasonal position of front in surface water is specified. (Author) Trans. of Gosudarstvennyi Okeanograficheskii Institut. Trudy (USSR) v79 p117-122 1966, by M. Slessers.

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