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    An Experimental Study of the Resonant Instability of an Internal Wave of Mode 3 Over a Range of Driving Frequencies

    Source: Journal of Physical Oceanography:;1974:;Volume( 004 ):;issue: 003::page 337
    Author:
    Hachmeister, Lon E.
    ,
    Martin, Seelye
    DOI: 10.1175/1520-0485(1974)004<0337:AESOTR>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: An experimental study of the stability of a progressive internal wave of mode 3 propagating down a long tank filled with a linearly stratified salt solution is conducted over the range 0.45≤?3/N≤0.80, where ?3 is the paddle frequency and N the Brunt-Väisälä frequency. Our observations show that the generated wave excites resonant triads at frequencies. below and forced triads at frequencies above the paddle frequency. There are two distinct families of resonant triads, corresponding to what Simmons calls set I and set II with modal form (n, n+3, 3) and (n+3, n, 3), n=1, 2, 3,?, respectively. Simmons' theory predicts that the set I triads grow approximately twice as fast as the corresponding triads of set II. In our experiments, we observe the set I triads at low amplitudes, with the set II triads forming as we increase the paddle amplitude. Above the driving frequency, we find only forced waves whose frequency and mode number are the sum of those of the paddle and the more energetic triad members, but whose wavenumber is not that of a free wave. The experiments substantiate Hasselmann's theoretical conjecture: that resonant instabilities alone cannot transfer energy to frequencies above the driving frequency.
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      An Experimental Study of the Resonant Instability of an Internal Wave of Mode 3 Over a Range of Driving Frequencies

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4162226
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    contributor authorHachmeister, Lon E.
    contributor authorMartin, Seelye
    date accessioned2017-06-09T14:43:55Z
    date available2017-06-09T14:43:55Z
    date copyright1974/07/01
    date issued1974
    identifier issn0022-3670
    identifier otherams-25442.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4162226
    description abstractAn experimental study of the stability of a progressive internal wave of mode 3 propagating down a long tank filled with a linearly stratified salt solution is conducted over the range 0.45≤?3/N≤0.80, where ?3 is the paddle frequency and N the Brunt-Väisälä frequency. Our observations show that the generated wave excites resonant triads at frequencies. below and forced triads at frequencies above the paddle frequency. There are two distinct families of resonant triads, corresponding to what Simmons calls set I and set II with modal form (n, n+3, 3) and (n+3, n, 3), n=1, 2, 3,?, respectively. Simmons' theory predicts that the set I triads grow approximately twice as fast as the corresponding triads of set II. In our experiments, we observe the set I triads at low amplitudes, with the set II triads forming as we increase the paddle amplitude. Above the driving frequency, we find only forced waves whose frequency and mode number are the sum of those of the paddle and the more energetic triad members, but whose wavenumber is not that of a free wave. The experiments substantiate Hasselmann's theoretical conjecture: that resonant instabilities alone cannot transfer energy to frequencies above the driving frequency.
    publisherAmerican Meteorological Society
    titleAn Experimental Study of the Resonant Instability of an Internal Wave of Mode 3 Over a Range of Driving Frequencies
    typeJournal Paper
    journal volume4
    journal issue3
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/1520-0485(1974)004<0337:AESOTR>2.0.CO;2
    journal fristpage337
    journal lastpage348
    treeJournal of Physical Oceanography:;1974:;Volume( 004 ):;issue: 003
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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