NON-STATIONARY TURBULENT REGIME IN THE SURFACE LAYER OF THE ATMOSPHERE.

Abstract

Regularities in the vertical distribution of wind and temperature are ascertained for non-stationary conditions in a region of small values of dimensionless height. The problem of the quasi-stationary transformation of the temperature field is studied as a function of changes in the shortwave insolation. The relationships obtained can be used in forecasting. (Author)

Document Details

Document Type
Technical Report
Publication Date
Dec 01, 1965
Accession Number
AD0628972

Entities

People

  • S. S. Zilitinkevich

Organizations

  • American Meteorological Society

Tags

DTIC Thesaurus Topics

  • Atmospheres
  • Delphi Method
  • Stationary

Readers

  • Fluid Dynamics.
  • Ocean-Atmosphere Mesoscale Modeling, Data Assimilation, and Flux Boundary Layers
  • Theoretical Analysis.