The dynamics of waves interacting with the Equatorial Undercurrent

We propose a new, simple model - but one which has far-reaching consequences - to describe the interaction between waves that propagate across the Pacific Ocean and the Equatorial Undercurrent (EUC). This involves a detailed discussion of the full linear problem as it relates to the dynamic coupling...

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Published inGeophysical and astrophysical fluid dynamics Vol. 109; no. 4; pp. 311 - 358
Main Authors Constantin, A, Johnson, R.S.
Format Journal Article
LanguageEnglish
Published Abingdon Taylor & Francis 04.07.2015
Taylor & Francis Ltd
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Abstract We propose a new, simple model - but one which has far-reaching consequences - to describe the interaction between waves that propagate across the Pacific Ocean and the Equatorial Undercurrent (EUC). This involves a detailed discussion of the full linear problem as it relates to the dynamic coupling between the surface waves and the internal waves on the thermocline. The result is a comprehensive description of the system close to the Equator, and how the structure of the EUC affects the wave properties; in particular, the analysis holds for arbitrary wavelengths and finite depths. Although the final expressions, for general wavelengths, are too cumbersome for direct interpretation, we are able to produce simple formulae for the speeds of the waves, and the attenuation factor between the two families of waves, for short, intermediate and long waves. Further, our results predict the appearance of critical layers under certain circumstances; by reverting to our original system of governing equations, we are able to derive the relevant nonlinear structure of the flow in these layers. Our results are in good agreement with the available field data.
AbstractList We propose a new, simple model - but one which has far-reaching consequences - to describe the interaction between waves that propagate across the Pacific Ocean and the Equatorial Undercurrent (EUC). This involves a detailed discussion of the full linear problem as it relates to the dynamic coupling between the surface waves and the internal waves on the thermocline. The result is a comprehensive description of the system close to the Equator, and how the structure of the EUC affects the wave properties; in particular, the analysis holds for arbitrary wavelengths and finite depths. Although the final expressions, for general wavelengths, are too cumbersome for direct interpretation, we are able to produce simple formulae for the speeds of the waves, and the attenuation factor between the two families of waves, for short, intermediate and long waves. Further, our results predict the appearance of critical layers under certain circumstances; by reverting to our original system of governing equations, we are able to derive the relevant nonlinear structure of the flow in these layers. Our results are in good agreement with the available field data.
Author Constantin, A
Johnson, R.S.
Author_xml – sequence: 1
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  orcidid: 0000-0001-8868-9305
  surname: Constantin
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  email: adrian.constantin@kcl.ac.uk
  organization: Faculty of Mathematics, University of Vienna
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  givenname: R.S.
  surname: Johnson
  fullname: Johnson, R.S.
  organization: School of Mathematics & Statistics, Newcastle University
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Snippet We propose a new, simple model - but one which has far-reaching consequences - to describe the interaction between waves that propagate across the Pacific...
We propose a new, simple model -- but one which has far-reaching consequences -- to describe the interaction between waves that propagate across the Pacific...
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SubjectTerms Attenuation
Computational fluid dynamics
Dispersion relation
Dynamical systems
Dynamics
Equatorial Undercurrent
Fluid dynamics
Mathematical analysis
Mathematical models
Ocean currents
Ocean waves
Pacific Ocean
Surface waves
Wave coupling
Waveform analysis
Wavelengths
Wind-drift current
Title The dynamics of waves interacting with the Equatorial Undercurrent
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