The Orographic Effects Induced by an Island Mountain Range on Propagating Tropical Cyclones.

Abstract

The orography effects on propagating tropical cyclone exerted by an idealized mesoscale, island mountain range was investigated by using a multi-layer primitive equation model with parameterized physics. The numerical simulation successfully reproduces the following observed behavior of the westward propagation tropical cyclones: (1) The intensity of the tropical cyclone is reduced; (2) the translating speed increases before passing the mountain ridge; (3) the storm center moves cyclonically in passing over the mountain; (4) the distribution of vertical motion is orographically modulated, upward motion occurs on the windside slopes where the vorticity is positive. The results indicated that the approaching tropical cyclone induces a cyclonic circulation around the topography. The mountain range constitutes a physical obstruction to the low-level flow and generates a strong easterly mass flow to the north of the mountain range.

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Document Details

Document Type
Technical Report
Publication Date
Oct 30, 1981
Accession Number
ADA106230

Entities

People

  • R. V. Madala
  • S. W. Chang

Organizations

  • United States Naval Research Laboratory

Tags

Communities of Interest

  • Energy and Power Technologies

DTIC Thesaurus Topics

  • Air Flow
  • Boundary Layer
  • Computational Science
  • Convection
  • Cyclones
  • Equations
  • Flow
  • Fluid Dynamics
  • Grids
  • Layers
  • Mass Flow
  • Meteorology
  • Physics
  • Simulations
  • Three Dimensional
  • Tropical Cyclones
  • Turbulence

Fields of Study

  • Environmental science

Readers

  • Atmospheric Science/Meteorology
  • Fluid Dynamics.