The Ocean in Motion by Manuel G. Velarde Roman Yu. Tarakanov & Alexey V. Marchenko

Author:Manuel G. Velarde, Roman Yu. Tarakanov & Alexey V. Marchenko
Language: eng
Format: epub
Publisher: Springer International Publishing, Cham

(115)

We see that the upper layer ageostrophic component is the superposition of long super-inertial internal waves considered in subsection “Linear Wave Modes”. The function does not contain the inertial oscillations (cf. subsection “Some Properties of the Ageostrophic Solution”) and at the interface any finite partial sum of the series (115) satisfies boundary conditions (111) with zero r.h.s. This means that in the very close vicinity of the interface the wave modes with very large numbers n play an important role. Since , vertical scales and frequencies of these modes are close to zero and to the inertial frequency, respectively. Joint effect of these modes forms the near interface boundary layer considered below in subsection “Boundary Layer”.

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