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    Equatorial Shelf Waves on an Exponential Shelf Profile

    Source: Journal of Physical Oceanography:;1978:;Volume( 008 ):;issue: 003::page 458
    Author:
    Mysak, Lawrence A.
    DOI: 10.1175/1520-0485(1978)008<0458:ESWOAE>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The theory of barotropic nondivergent waves trapped on an exponential shelf lying on an equatorial ?-plane is presented. The bottom contours are parallel to the equator so that phase propagation is either eastward or westward. according to the following general rule: when the shelf region is entirely in the Northern (Southern) Hemisphere the shallow water is to the right (left) of the direction of the phase velocity. When both the shelf and deep sea regions are located in the same hemisphere (case 1), the results concerning the dispersion curves and eigenfunctions are qualitatively similar to those obtained by Buch-wald and Adams (1968) for shelf waves on a mid-latitude exponential shelf on an f-plane. However, when the shelf region is on one side of the equator and the deep sea region extends across the equator (case 2), the dispersion curves and eigenfunctions are quite different. In case 2 the dispersion curve for each trapped mode has a long-wave cutoff. However, the cutoff for each mode generally does not preclude the existence of a zero group velocity at an intermediate wavelength. a phenomenon which always occurs in case 1. In case 2 the range of oscillation for each eigenfunction is generally much larger than that of the corresponding eigenfunction in case 1. Finally, when the shelf region straddles the equator (case 3), both westward and eastward propagating modes may exist. Further, one set of these modes has a long-wave cutoff (e.g., if the coast is in the Southern Hemisphere with deep water to the north, the westward propagating modes have a long-wave cutoff). In case 3 the oscillations of each eigenfunction tend to be concentrated near the shelf edge. The theory is applied to the Gulf of Guinea. where a 0.07 cycle per day (cpd) oscillation in the sea surface temperature has been observed to propagate westward along the Ghaina-lyory coast. It is shown that this signal may be due to the presence of a fundamental mode shelf wave of the type discussed in this paper.
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      Equatorial Shelf Waves on an Exponential Shelf Profile

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4162636
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    contributor authorMysak, Lawrence A.
    date accessioned2017-06-09T14:44:46Z
    date available2017-06-09T14:44:46Z
    date copyright1978/05/01
    date issued1978
    identifier issn0022-3670
    identifier otherams-25811.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4162636
    description abstractThe theory of barotropic nondivergent waves trapped on an exponential shelf lying on an equatorial ?-plane is presented. The bottom contours are parallel to the equator so that phase propagation is either eastward or westward. according to the following general rule: when the shelf region is entirely in the Northern (Southern) Hemisphere the shallow water is to the right (left) of the direction of the phase velocity. When both the shelf and deep sea regions are located in the same hemisphere (case 1), the results concerning the dispersion curves and eigenfunctions are qualitatively similar to those obtained by Buch-wald and Adams (1968) for shelf waves on a mid-latitude exponential shelf on an f-plane. However, when the shelf region is on one side of the equator and the deep sea region extends across the equator (case 2), the dispersion curves and eigenfunctions are quite different. In case 2 the dispersion curve for each trapped mode has a long-wave cutoff. However, the cutoff for each mode generally does not preclude the existence of a zero group velocity at an intermediate wavelength. a phenomenon which always occurs in case 1. In case 2 the range of oscillation for each eigenfunction is generally much larger than that of the corresponding eigenfunction in case 1. Finally, when the shelf region straddles the equator (case 3), both westward and eastward propagating modes may exist. Further, one set of these modes has a long-wave cutoff (e.g., if the coast is in the Southern Hemisphere with deep water to the north, the westward propagating modes have a long-wave cutoff). In case 3 the oscillations of each eigenfunction tend to be concentrated near the shelf edge. The theory is applied to the Gulf of Guinea. where a 0.07 cycle per day (cpd) oscillation in the sea surface temperature has been observed to propagate westward along the Ghaina-lyory coast. It is shown that this signal may be due to the presence of a fundamental mode shelf wave of the type discussed in this paper.
    publisherAmerican Meteorological Society
    titleEquatorial Shelf Waves on an Exponential Shelf Profile
    typeJournal Paper
    journal volume8
    journal issue3
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/1520-0485(1978)008<0458:ESWOAE>2.0.CO;2
    journal fristpage458
    journal lastpage467
    treeJournal of Physical Oceanography:;1978:;Volume( 008 ):;issue: 003
    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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