A Simple Model of the Thermocline in a Bounded Ocean

dc.contributor.author	Barcilon, Victor
dc.date.accessioned	2017-06-09T14:43:26Z
dc.date.available	2017-06-09T14:43:26Z
dc.date.copyright	1971/01/01
dc.date.issued	1971
dc.identifier.issn	0022-3670
dc.identifier.other	ams-25245.pdf
dc.identifier.uri	http://onlinelibrary.yabesh.ir/handle/yetl/4162007
dc.description.abstract	A linear model of the thermocline is examined for an ocean bounded by both eastern and western coasts. The analysis is carried out on a ?-plane for an ocean in which diffusion of heat but not of momentum is important. Particular attention is devoted to the structure of the thermocline in the vicinity of the western coast along which a boundary layer exists. A unique feature of the present thermocline is the absence of any vertical velocity below the thermocline.
dc.publisher	American Meteorological Society
dc.title	A Simple Model of the Thermocline in a Bounded Ocean
dc.type	Journal Paper
dc.journal.volume	1
dc.journal.issue	1
dc.journal.title	Journal of Physical Oceanography
dc.identifier.doi	10.1175/1520-0485(1971)001<0007:ASMOTT>2.0.CO;2
dc.journal.fristpage	7
dc.journal.lastpage	11
dc.tree	Journal of Physical Oceanography:;1971:;Volume( 001 ):;issue: 001
dc.contenttype	Fulltext