Generation of Internal Waves by a Moving Region of Pressures in a Sea with a Discountinuity Layer (Gereratsiya Vnutrennikh voln Divzhushcheysya Oblast'yu Davleniy v More so Sloyem Skachka),

Abstract

Steady internal waves in a sea, caused by displacement of a region of baric disturbances, are investigated. The continuous density stratification is such that the Vaisala-Brunt frequency is zero in the upper and lower layers and positive in the middle layer (discontinuity layer). (Author)

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Document Details

Document Type
Technical Report
Publication Date
Feb 01, 1977
Accession Number
ADA036887

Entities

People

  • L. V. Cherkeson
  • S. F. Dotsenko

Organizations

  • Office of Naval Intelligence

Tags

Communities of Interest

  • C4I
  • Energy and Power Technologies

DTIC Thesaurus Topics

  • Amplitude
  • Coordinate Systems
  • Demographic Cohorts
  • Discontinuities
  • Equations
  • Frequency
  • Internal Waves
  • Intervals
  • Layers
  • Naval Intelligence
  • Numerical Analysis
  • Resonance
  • Solitons
  • Stratified Fluids
  • Surface Waves
  • Thickness
  • Waves

Readers

  • Atmospheric Science / Meteorology, specifically Wind Wave Turbulence.
  • Information Retrieval