THE VERTICAL INFLUENCE OF DYNAMIC DISTURBANCES BETWEEN THE STRATOSPHERE AND THE TROPOSPHERE,

Abstract

The solution of the vertical velocity equation derived from the vorticity and thermodynamic equations with the stratospheric effect taken into consideration shows that the disturbances in the stratosphere with a longer wavelength can produce a slight effect on the troposphere but the effect of those with a shorter wavelength can hardly reach that part of the atmosphere. The effect of the disturbances in the troposphere with a longer wavelength on the stratosphere is greater than that in the stratosphere on itself. These effects are equal in the case of a shorter wavelength.

Document Details

Document Type
Technical Report
Publication Date
Oct 01, 1966
Accession Number
AD0644565

Entities

People

  • Chen Yung-san

Organizations

  • Emmanuel College

Tags

DTIC Thesaurus Topics

  • Atmosphere (Earth)
  • Atmospheres
  • Biological Phenomena
  • Ecological And Environmental Phenomena
  • Environment
  • Equations
  • Republic
  • Stratosphere
  • Troposphere

Fields of Study

  • Environmental science

Readers

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

Technology Areas

  • Space