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    Generation and Growth Mechanism of the Natal Pulse

    Source: Journal of Physical Oceanography:;2010:;Volume( 040 ):;issue: 007::page 1597
    Author:
    Tsugawa, Motohiko
    ,
    Hasumi, Hiroyasu
    DOI: 10.1175/2010JPO4347.1
    Publisher: American Meteorological Society
    Abstract: The 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.
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      Generation and Growth Mechanism of the Natal Pulse

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4212766
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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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    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
    yabeshDSpacePersian