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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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