In:
Journal of Geophysical Research: Oceans, American Geophysical Union (AGU), Vol. 94, No. C3 ( 1989-03-15), p. 3223-3227
Abstract:
During February 1988 a layer of almost uniform temperature and salinity between 100 and 1250 m depth was observed in the central Greenland Sea. This feature, indicative of previous deep convection, is explained in terms of a conceptual penetrative convection model.
Type of Medium:
Online Resource
ISSN:
0148-0227
DOI:
10.1029/JC094iC03p03223
Language:
English
Publisher:
American Geophysical Union (AGU)
Publication Date:
1989
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