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    Why Are There Agulhas Rings?

    Source: Journal of Physical Oceanography:;1999:;Volume( 029 ):;issue: 004::page 693
    Author:
    Pichevin, Thierry
    ,
    Nof, Doron
    ,
    Lutjeharms, Johann
    DOI: 10.1175/1520-0485(1999)029<0693:WATAR>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The recently proposed analytical theory of Nof and Pichevin describing the intimate relationship between retroflecting currents and the production of rings is examined numerically and applied to the Agulhas Current. Using a reduced-gravity 1½-layer primitive equation model of the Bleck and Boudra type the authors show that, as the theory suggests, the generation of rings from a retroflecting current is inevitable. The generation of rings is not due to an instability associated with the breakdown of a known steady solution but rather is due to the zonal momentum flux (i.e., flow force) of the Agulhas jet that curves back on itself. Numerical experiments demonstrate that, to compensate for this flow force, several rings are produced each year. Since the slowly drifting rings need to balance the entire flow force of the retroflecting jet, their length scale is considerably larger than the Rossby radius; that is, their scale is greater than that of their classical counterparts produced by instability. Recent observations suggest a correlation between the so-called ?Natal Pulse? and the production of Agulhas rings. As a by-product of the more general retroflection experiments, the pulse issue is also examined numerically using two different representations for the pulses. The first is a meander pulse (i.e., the pulse is similar to a meander) and the second is a transport pulse. It is shown that, in this model, there is no obvious relationship between the presence of Natal pulses and the production of rings.
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      Why Are There Agulhas Rings?

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4166189
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    contributor authorPichevin, Thierry
    contributor authorNof, Doron
    contributor authorLutjeharms, Johann
    date accessioned2017-06-09T14:53:22Z
    date available2017-06-09T14:53:22Z
    date copyright1999/04/01
    date issued1999
    identifier issn0022-3670
    identifier otherams-29009.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4166189
    description abstractThe recently proposed analytical theory of Nof and Pichevin describing the intimate relationship between retroflecting currents and the production of rings is examined numerically and applied to the Agulhas Current. Using a reduced-gravity 1½-layer primitive equation model of the Bleck and Boudra type the authors show that, as the theory suggests, the generation of rings from a retroflecting current is inevitable. The generation of rings is not due to an instability associated with the breakdown of a known steady solution but rather is due to the zonal momentum flux (i.e., flow force) of the Agulhas jet that curves back on itself. Numerical experiments demonstrate that, to compensate for this flow force, several rings are produced each year. Since the slowly drifting rings need to balance the entire flow force of the retroflecting jet, their length scale is considerably larger than the Rossby radius; that is, their scale is greater than that of their classical counterparts produced by instability. Recent observations suggest a correlation between the so-called ?Natal Pulse? and the production of Agulhas rings. As a by-product of the more general retroflection experiments, the pulse issue is also examined numerically using two different representations for the pulses. The first is a meander pulse (i.e., the pulse is similar to a meander) and the second is a transport pulse. It is shown that, in this model, there is no obvious relationship between the presence of Natal pulses and the production of rings.
    publisherAmerican Meteorological Society
    titleWhy Are There Agulhas Rings?
    typeJournal Paper
    journal volume29
    journal issue4
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/1520-0485(1999)029<0693:WATAR>2.0.CO;2
    journal fristpage693
    journal lastpage707
    treeJournal of Physical Oceanography:;1999:;Volume( 029 ):;issue: 004
    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
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