The Saudi Arabian Heat Low: A Numerical Perspective.

Abstract

Results are presented from several numerical experiments designed to simulate the Saudi Arabian 'heat low' and to test the sensitivity of the 'heat low' circulation to certain parameters. Data collected during the Summer Monsoon Experiment (1979) are analyzed to obtain vertical and temporal distributions of temperature, water vapor mixing ratio, and dust mass loading. These distributions, along with climatological vertical profiles of ozone and carbon dioxide, are used as input to broadband longwave and shortwave radiative transfer routines to obtain radiative heating rates over the Saudi Arabian desert and the western Arabian Sea for both clear and dust laden desert is parameterized by the net radiation at the desert surface. The sensible heat is vertically distributed over the desert according to the diurnal pattern of mixed layer growth as determined by a 1-dimensional mixed layer growth model. The horizontal gradients in the vertical distributions of radiative and sensible heating between the desert and the ocean are used to force a 2-dimensional, axisymmetric, dry, primitive equation model to simulate the 'heat low' circulation.

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Document Details

Document Type
Technical Report
Publication Date
Jan 01, 1984
Accession Number
ADA145575

Entities

People

  • L. E. Freeman

Organizations

  • Air Force Institute of Technology

Tags

Communities of Interest

  • Energy and Power Technologies

DTIC Thesaurus Topics

  • Air Force
  • Arabian Sea
  • Atmospheric Sciences
  • Boundary Layer
  • Energy
  • Energy Transfer
  • Geography
  • Grids
  • Heat Capacity
  • Heat Transfer
  • Intervals
  • Measurement
  • Meteorology
  • Specific Heat
  • Stratified Fluids
  • Three Dimensional
  • Water Vapor

Fields of Study

  • Environmental science

Readers

  • Aerosol Science/Aerosol Physics
  • Atmospheric Science/Meteorology
  • Ocean-Atmosphere Mesoscale Modeling, Data Assimilation, and Flux Boundary Layers