On the possibility of convective overturning in the Słupsk Furrow overflow of the Baltic Sea
Alosely spaced CTD transects across the Slupsk Furrow displayed a "downward-bending" of salinity contours below the salinity interface on the southern flank due to a transverse circulation in the saline water overflow. Numerical simulation of a gravity current in an idealized channel with...
Main Authors: | , , , , , , , |
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Format: | Article |
Language: | English |
Published: |
Elsevier
2011-09-01
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Series: | Oceanologia |
Subjects: | |
Online Access: | http://www.iopan.gda.pl/oceanologia/53_3.html#A6 |