contributor author | Smith, Neville R. | |
contributor author | Fandry, C. B. | |
date accessioned | 2017-06-09T14:44:11Z | |
date available | 2017-06-09T14:44:11Z | |
date copyright | 1976/01/01 | |
date issued | 1976 | |
identifier issn | 0022-3670 | |
identifier other | ams-25565.pdf | |
identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4162362 | |
description abstract | A simple, frictional, linear model is used to study the motion of the Gull Stream over the continental shelf. It is found that the combination of frictional and topographic effects may provide a further mechanism by which the observed separation of the Gulf Stream may be achieved. The model predicts separation in the form of a classical separated boundary layer and interrelates the slope of the bottom with the position of separation. Counter-circulations northwest of the stream and increased northward transport of the current are also predicted. | |
publisher | American Meteorological Society | |
title | A Simple Topographic Model of Gulf Stream Separation | |
type | Journal Paper | |
journal volume | 6 | |
journal issue | 1 | |
journal title | Journal of Physical Oceanography | |
identifier doi | 10.1175/1520-0485(1976)006<0022:ASTMOG>2.0.CO;2 | |
journal fristpage | 22 | |
journal lastpage | 28 | |
tree | Journal of Physical Oceanography:;1976:;Volume( 006 ):;issue: 001 | |
contenttype | Fulltext | |