Analytic Modeling of Severe Vortical Storms.

Abstract

The analytic modeling of well-organized rotating convective storms is invoked to elucidate the evolution from a moderately intense one-cell vortex, characterized by low-level pressure deficits on the order of one percent of atmospheric pressure, to a very intense two-cell vortex, characterized by low-level pressure deficits on the order of ten percent of atmospheric pressure. The physical distinction between the two stages rests on the insertion of a dry, compressionally heated, nonrotating, central downdraft of originally tropopause-level air in the transition to the more severe case. The quasisteady mature description of the thermohydrodynamic structure of each vortex is being developed, and then the conditions for transition from the moderately intense to the very intense vortex will be sought. The practical motivation is to make progress toward the highly desirable, but very formidable task of being able to anticipate which tropical storms or minimal hurricanes will evolve to supertyphoons. With a description of the one-cell storm, believed adequate for present purposes, already available, description of the two-cell vortex is the current challenge.

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Document Details

Document Type
Technical Report
Publication Date
Oct 01, 1981
Accession Number
ADA107706

Entities

People

  • Francis E. Fendell
  • George Carrier
  • Phillip Feldman

Tags

Communities of Interest

  • Air Platforms
  • Materials and Manufacturing Processes
  • Space

DTIC Thesaurus Topics

  • Angular Momentum
  • Barometric Pressure
  • Boundary Layer
  • Boundary Value Problems
  • Cell Structure
  • Computational Fluid Dynamics
  • Computational Science
  • Cyclones
  • Fluid Dynamics
  • Heat Energy
  • Layers
  • Pressure Distribution
  • Pressure Gradients
  • Sea Level
  • Space Systems
  • Transitions
  • Tropical Cyclones

Readers

  • Atmospheric Science/Meteorology
  • Fluid Mechanics and Fluid Dynamics.
  • Systems Analysis and Design