A Model Study of Changes in Wind With Altitude in a Planetary Boundary Layer

Abstract

The paper presents a solution from which the majority of the known solutions are derived as partial cases. These equations and models are used in studying the time-wise changes in wind with height in the planetary boundary layer. Here K(z) is the kinematic coefficient of turbulent exchange along the z axis and liter is the Coriolis force.

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Document Details

Document Type
Technical Report
Publication Date
Aug 15, 1969
Accession Number
AD0863433

Entities

People

  • D. Iordanov
  • N. Godev

Tags

DTIC Thesaurus Topics

  • Altitude
  • Boundaries
  • Boundary Layer
  • Coefficients
  • Contractors
  • Contracts
  • Equations
  • Export Controls
  • Foreign Technology
  • Layers
  • Translations

Fields of Study

  • Physics

Readers

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