A PRELIMINARY STUDY OF THE INSTABILITY AND DEVELOPMENT OF ULTRA-LONG WAVES,

Abstract

The instability and development of ultra-long waves under frictionless and adiabatic conditions are discussed. The vertical distribution of the static stability and the vertical wind shear of the basic current are found to be factors controlling the instability of ultra-long waves. The occurrence of instability requires that the environmental static stability increases with height and this condition is fulfilled in the atmosphere by virtue of the existence of the stratosphere. The greater the magnitude of the vertical wind shear, the higher is the degree of instability of these waves. Equations relating the vertical wind shear of the basic current to the variation of static stability are derived on the assumption that the disturbances exert a 'feedback' effect on the basic current. This effect is much more pronounced on vertical wind shear than static stability. In addition to the vertical wind shear of the basic current and the vertical distribution of static stability, the wavelength also affects the development of ultra-long waves though this parameter does not affect the maximum amplitude of the mature disturbance. However, the longer the wavelength, the longer it takes for the disturbance to fully develop. The presence of the stratosphere tends to reduce the amplitude of mature disturbances at low levels and enhance those at high levels. (Author)

Document Details

Document Type
Technical Report
Publication Date
Mar 01, 1969
Accession Number
AD0686238

Entities

People

  • Wang Hsiao-ling
  • Yeh Tu-cheng

Organizations

  • Emmanuel College

Tags

DTIC Thesaurus Topics

  • Adiabatic Conditions
  • Amplitude
  • Atmospheres
  • Equations
  • Feedback
  • Instability
  • Stratosphere
  • Wind
  • Wind Shear

Readers

  • Atmospheric Science/Meteorology
  • Fluid Dynamics.
  • Systems Analysis and Design

Technology Areas

  • Space