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contributor authorTsugawa, Motohiko
contributor authorHasumi, Hiroyasu
date accessioned2017-06-09T16:36:49Z
date available2017-06-09T16:36:49Z
date copyright2010/07/01
date issued2010
identifier issn0022-3670
identifier otherams-70931.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4212766
description abstractThe Natal pulses, solitary cyclonic meanders in the Agulhas Current, are reproduced in an ocean general circulation model. The model covers the region around the Agulhas Current with a grid fine enough to reproduce major eddies. The features of the reproduced Natal pulses are consistent with observational evidences in the following respects: they are generated at the Natal Bight when anticyclonic eddies come, move downstream along the Agulhas Current at speeds about 20 km day?1, and grow in its horizontal size as they move. The present simulation shows that the generation and growth of the Natal pulse occurs because of the interaction between the mean flow of the Agulhas Current and an anticyclonic eddy. A supplemental simulation, where the topography of the Natal Bight is modified, indicates that the topography of the Natal Bight does not cause the generation of the Natal pulses, contrary to a previous suggestion.
publisherAmerican Meteorological Society
titleGeneration and Growth Mechanism of the Natal Pulse
typeJournal Paper
journal volume40
journal issue7
journal titleJournal of Physical Oceanography
identifier doi10.1175/2010JPO4347.1
journal fristpage1597
journal lastpage1612
treeJournal of Physical Oceanography:;2010:;Volume( 040 ):;issue: 007
contenttypeFulltext


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