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    Standing Equatorial Wave Modes in Bounded Ocean Basins

    Source: Journal of Physical Oceanography:;1979:;Volume( 009 ):;issue: 004::page 653
    Author:
    Gent, Peter R.
    DOI: 10.1175/1520-0485(1979)009<0653:SEWMIB>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A new type of standing equatorial wave mode is described that exists in the semi-infinite ocean 0 ? x ? L, ?∞ ? y ? ∞. It consists of a finite sum of the meridionally trapped equatorial waves in an infinite x domain. The new mode is thus itself equatorially trapped and requires no energy sources or sinks at |y| = ∞. However, it exists only for a discrete, countable set of pairs of values of the frequency ? and the ocean zonal width L. Previously described standing modes exist for any ocean width, but are infinite sums of trapped equatorial waves and require a continuous energy source in the west at |y| = ∞ to balance the continuous energy sink in the east at |y| = ∞. Several examples of the new type of standing mode are given, and it is shown that as the standing mode period becomes very long, so the zonal scale becomes very short. The effect on the standing modes of bounding the basin meridionally is also described; energy is recycled round the basin by boundary-trapped Kelvin waves along the zonal walls. The amount of energy recycled in the new type of standing mode, however, is exponentially small compared to that recycled in the previously described standing modes.
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      Standing Equatorial Wave Modes in Bounded Ocean Basins

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4162782
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    contributor authorGent, Peter R.
    date accessioned2017-06-09T14:45:08Z
    date available2017-06-09T14:45:08Z
    date copyright1979/07/01
    date issued1979
    identifier issn0022-3670
    identifier otherams-25943.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4162782
    description abstractA new type of standing equatorial wave mode is described that exists in the semi-infinite ocean 0 ? x ? L, ?∞ ? y ? ∞. It consists of a finite sum of the meridionally trapped equatorial waves in an infinite x domain. The new mode is thus itself equatorially trapped and requires no energy sources or sinks at |y| = ∞. However, it exists only for a discrete, countable set of pairs of values of the frequency ? and the ocean zonal width L. Previously described standing modes exist for any ocean width, but are infinite sums of trapped equatorial waves and require a continuous energy source in the west at |y| = ∞ to balance the continuous energy sink in the east at |y| = ∞. Several examples of the new type of standing mode are given, and it is shown that as the standing mode period becomes very long, so the zonal scale becomes very short. The effect on the standing modes of bounding the basin meridionally is also described; energy is recycled round the basin by boundary-trapped Kelvin waves along the zonal walls. The amount of energy recycled in the new type of standing mode, however, is exponentially small compared to that recycled in the previously described standing modes.
    publisherAmerican Meteorological Society
    titleStanding Equatorial Wave Modes in Bounded Ocean Basins
    typeJournal Paper
    journal volume9
    journal issue4
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/1520-0485(1979)009<0653:SEWMIB>2.0.CO;2
    journal fristpage653
    journal lastpage662
    treeJournal of Physical Oceanography:;1979:;Volume( 009 ):;issue: 004
    contenttypeFulltext
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