Dynamically Driven Roll Circulations in an Inversion-Capped Boundary Layer

Abstract

From a Boussinesq system of equations modified to include background wind and temperature profiles, a two-dimensional, nonlinear spectral model is derived to study the development of boundary layer roll circulations in a nonrotating, stratified environment. The spectral expansions for the dependent variables include more than one vertical harmonic, thereby allowing the determination of the structure of the roll circulations and the roles of the dynamic and thermodynamic instability mechanisms. The dynamic forcing is represented by a Fourier expansion of an arbitrary vertical profile of the background horizontal wind. In this theses, only the linear aspects of the roll solutions are examined through the use of a standard linear stability analysis. From this analysis are obtained the minimum critical values of the dynamic forcing parameter Re and the effective thermodynamic forcing parameter Ra sub e that represent the smallest magnitudes of the forcing rates required for the onset of roll circulations. In addition, the preferred horizontal wavelengths, circulation depths and orientations with respect to a reference direction are found for the various roll modes. (JHD)

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Document Details

Document Type
Technical Report
Publication Date
Aug 01, 1989
Accession Number
ADA228918

Entities

People

  • Robert Medred

Organizations

  • Air Force Institute of Technology

Tags

Communities of Interest

  • Energy and Power Technologies

DTIC Thesaurus Topics

  • Air Force
  • Boundary Layer
  • Climate Change
  • Convection
  • Coordinate Systems
  • Differential Equations
  • Energy Transfer
  • Geometry
  • Lapse Rate
  • Meteorology
  • Partial Differential Equations
  • Pennsylvania
  • Temperature Gradients
  • Temperature Inversion
  • Thermal Instability
  • Two Dimensional
  • Wind Direction

Readers

  • Control Systems Engineering.
  • Ocean-Atmosphere Mesoscale Modeling, Data Assimilation, and Flux Boundary Layers