Sub-inertial modulation of nonlinear Kelvin waves in the coastal zone

Observational evidence is presented for interaction between nonlinear internal Kelvin waves at the &omega;<sub>t,i</sub> (where the &omega;<sub>t</sub> is the semidiurnal frequency and the &omega;<sub>i</sub> is the inertial frequency) and random oscil...

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Bibliographic Details
Main Authors: D. V. Stepanov, V. V. Novotryasov
Format: Article
Language:English
Published: Copernicus Publications 2013-06-01
Series:Nonlinear Processes in Geophysics
Online Access:http://www.nonlin-processes-geophys.net/20/357/2013/npg-20-357-2013.pdf
Description
Summary:Observational evidence is presented for interaction between nonlinear internal Kelvin waves at the &omega;<sub>t,i</sub> (where the &omega;<sub>t</sub> is the semidiurnal frequency and the &omega;<sub>i</sub> is the inertial frequency) and random oscillations of the background coastal current at the sub-inertial Ω frequency in the Japan/East Sea. Enhanced coastal currents at the sum &omega;<sub>+</sub> and difference ω-frequencies &omega;<sub>&plusmn;</sub>=&omega;<sub>t,i</sub> &plusmn; &Omega; have properties of propagating Kelvin waves, which suggests permanent energy exchange from the sub-inertial band to the mesoscale &omega;<sub>&plusmn;</sub> band. This interaction may be responsible for a greater-than-predicted intensification, steepening and breaking of boundary-trapped Kelvin waves. The problem of interaction between the nonlinear Kelvin wave at the frequency &omega; and the low-frequency narrowband noise with representative frequency &Omega;&ll;&omega; is investigated using the theory of nonlinear weak dispersion waves.
ISSN:1023-5809
1607-7946