Numerical Simulation of Wind, Temperature, Shear Stress and Turbulent Energy over Nonhomogeneous Terrain.

Abstract

Airflow in the atmospheric surface layer over nonhomogeneous surfaces with discontinuities in surface roughness and temperature is investigated by numerical techniques. A computational scheme is developed for solving the steady state two-dimensional boundary layer equations. Several theorems of convergence are proved. A successful numerical test, which has been compared to the exact solution, is achieved. Some iterative schemes, which have already enjoyed considerable success without theoretical support are here shown to be convergent. The variations in pressure and buoyancy force associated with changes in surface roughness have been neglected by previous investigators whose work is included in the present study. The numerical results of velocity and shear stress are compared with wind tunnel and field data. The roughness and temperature discontinuities are shown to have an effect on the upstream as well as the downstream flow conditions. (Author)

Document Details

Document Type
Technical Report
Publication Date
Mar 01, 1972
Accession Number
AD0751589

Entities

People

  • Chin-hua Huang
  • E. C. Nickerson

Organizations

  • Colorado State University

Tags

DTIC Thesaurus Topics

  • Boundary Layer
  • Discontinuities
  • Downstream Flow
  • Layers
  • Roughness
  • Shear Stresses
  • Simulations
  • Steady State
  • Stresses
  • Surface Roughness
  • Two Dimensional
  • Wind Tunnels

Fields of Study

  • Mathematics

Readers

  • Calculus or Mathematical Analysis
  • Computational Fluid Dynamics (CFD)
  • Fluid Dynamics.