Internal Waves in a Lagrangian Reference Frame

Abstract

Several recent studies of internal gravity waves have been expressed in a Lagrangian reference frame, motivated by the observation that in this frame the dispersion relation then excludes the Eulerian Doppler shifting term due to a background flow. Here the dispersion relation in a Lagrangian reference frame is explicitly derived for a background flow and background density that are slowly varying with respect to the waves, but are otherwise arbitrary functions of space and time. Two derivations are given, both yielding the same result. The first derivation involves a transformation of the dispersion relation from Eulerian to Lagrangian coordinates, while the second derivation involves a wave-packet analysis of the equations of motion directly in Lagrangian coordinates. The authors show that, although the Eulerian Doppler shifting term is removed from the dispersion relation by the transformation of the frequency when passing from an Eulerian to a Lagrangian reference frame, a dependence on the background shear is then introduced by the transformation of the wavenumber. This dependence on the background shear is the term that accounts for wave refraction in the Lagrangian frame, and its role has apparently not been fully appreciated in the aforementioned previous studies.

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Document Details

Document Type
Technical Report
Publication Date
Jun 01, 2004
Accession Number
ADA524821

Entities

People

  • Dave Broutman
  • Roger H. Grimshaw
  • Stephen D. Eckermann

Organizations

  • United States Naval Research Laboratory

Tags

DTIC Thesaurus Topics

  • Abstracts
  • Coordinate Systems
  • Differential Equations
  • Dispersion Relations
  • Dispersions
  • Equations
  • Equations Of Motion
  • Frequency
  • Gravity
  • Gravity Waves
  • Group Velocity
  • Internal Waves
  • Military Research
  • Partial Differential Equations
  • Refraction
  • Wave Packets
  • Waves

Readers

  • Atmospheric Science / Meteorology, specifically Wind Wave Turbulence.
  • Finite Element Method (FEM) for solving Partial Differential Equations (PDEs)
  • Geodesy

Technology Areas

  • Space