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contributor authorButman, B.
contributor authorBeardsley, R. C.
contributor authorMagnell, B.
contributor authorFrye, D.
contributor authorVermersch, J. A.
contributor authorSchlitz, R.
contributor authorLimeburner, R.
contributor authorWright, W. R.
contributor authorNoble, M. A.
date accessioned2017-06-09T14:46:11Z
date available2017-06-09T14:46:11Z
date copyright1982/06/01
date issued1982
identifier issn0022-3670
identifier otherams-26365.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4163251
description abstractA clockwise circulation around Georges Bank was measured by means of moored current meters, aircraft-tracked surface drifters, and satellite-tracked drifters drogued at 10 m. The strongest flow was in a narrow jetlike current (30 cm s?1) along the northern flank of the bank. The flow of shelf water on the southern flank was westward (10 cm s?1) toward the Middle Atlantic Bight; some of this water flowed northward through the eastern side of Great South Channel and recirculated around Georges Bank. The satellite-tracked drifters and the moored observations indicate that the circulation around the bank was not completely closed and considerable variability occurs in the trajectory of an individual water particle.
publisherAmerican Meteorological Society
titleRecent Observations of the Mean Circulation on Georges Bank
typeJournal Paper
journal volume12
journal issue6
journal titleJournal of Physical Oceanography
identifier doi10.1175/1520-0485(1982)012<0569:ROOTMC>2.0.CO;2
journal fristpage569
journal lastpage591
treeJournal of Physical Oceanography:;1982:;Volume( 012 ):;issue: 006
contenttypeFulltext


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