Repository logo
  • English
  • Català
  • Čeština
  • Deutsch
  • Español
  • Français
  • Gàidhlig
  • Italiano
  • Latviešu
  • Magyar
  • Nederlands
  • Polski
  • Português
  • Português do Brasil
  • Suomi
  • Svenska
  • Türkçe
  • Қазақ
  • বাংলা
  • हिंदी
  • Ελληνικά
  • Yкраї́нська
  • Log In
    or
    New user? Click here to register.Have you forgotten your password?
Repository logo
  • Communities & Collections
  • Research Outputs
  • Fundings & Projects
  • People
  • Statistics
  • English
  • Català
  • Čeština
  • Deutsch
  • Español
  • Français
  • Gàidhlig
  • Italiano
  • Latviešu
  • Magyar
  • Nederlands
  • Polski
  • Português
  • Português do Brasil
  • Suomi
  • Svenska
  • Türkçe
  • Қазақ
  • বাংলা
  • हिंदी
  • Ελληνικά
  • Yкраї́нська
  • Log In
    or
    New user? Click here to register.Have you forgotten your password?
  1. Home
  2. Indian Institute of Technology Madras
  3. Publication2
  4. Triadic resonances in internal wave modes with background shear
 
  • Details
Options

Triadic resonances in internal wave modes with background shear

Date Issued
25-12-2021
Author(s)
Patibandla, Ramana
Manikandan Mathur 
Indian Institute of Technology, Madras
Anubhab Roy 
Indian Institute of Technology, Madras
DOI
10.1017/jfm.2021.847
Abstract
In this paper, we use asymptotic theory and numerical methods to study resonant triad interactions among discrete internal wave modes at a fixed frequency in a two-dimensional, uniformly stratified shear flow. Motivated by linear internal wave generation mechanisms in the ocean, we assume the primary wave field as a linear superposition of various horizontally propagating vertical modes at a fixed frequency. The weakly nonlinear solution associated with the primary wave field is shown to comprise superharmonic (frequency) and zero frequency wave fields, with the focus of this study being on the former. When two interacting primary modes and are in triadic resonance with a superharmonic mode, it results in the divergence of the corresponding superharmonic secondary wave amplitude. For a given modal interaction, the superharmonic wave amplitude is plotted on the plane of primary wave frequency and Richardson number, and the locus of divergence locations shows how the resonance locations are influenced by background shear. In the limit of weak background shear , using an asymptotic theory, we show that the horizontal wavenumber condition is sufficient for triadic resonance, in contrast to the requirement of an additional vertical mode number condition in the case of no shear. As a result, the number of resonances for an arbitrarily weak shear is significantly larger than that for no shear. The new resonances that occur in the presence of shear include the possibilities of resonance due to self-interaction and resonances that occur at the seemingly trivial limit of, both of which are not possible in the no shear limit. Our weak shear limit conclusions are relevant for other inhomogeneities such as non-uniformity in stratification as well, thus providing an understanding of several recent studies that have highlighted superharmonic generation in non-uniform stratifications. Extending our study to finite shear (finite) in an ocean-like exponential shear flow profile, we show that for cograde-cograde interactions, a significant number of divergence curves that start at will not extend below a cutoff. In contrast, for retrograde-retrograde interactions, the divergence curves extend all the way from to. For mixed interactions, new divergence curves appear at for and extend to other primary wave frequencies for smaller. Consequently, the total number of resonant triads is of the same order for small as in the limit of weak shear , although it attains a maximum at.
Volume
929
Subjects
  • Key words internal wa...

  • stratified flows

Indian Institute of Technology Madras Knowledge Repository developed and maintained by the Library

Built with DSpace-CRIS software - Extension maintained and optimized by 4Science

  • Cookie settings
  • Privacy policy
  • End User Agreement
  • Send Feedback