The ROSCOE Manual. Volume 16. High-Altitude Neutral-Particle Motion.

Abstract

Two preliminary, alternative models of the high-altitude (h > or = 90 km) neutral-particle motion have been adopted for use in ROSCOE. Both models are one-dimensional spherical Lagrangian models and describe the vertical hydrodynamic motion in each geocentric column in an array of perhaps 100 such continuous but independent columns covering the disturbed region of interest. The models (SAIHYD, NRLHYD) describe the motion of a set of either Lagrangian cells or points by using the method of either difference equations or differential quadrature, respectively. Both models have automatic rezone capability. The geocentric columns defining the geometry for the calculations are described in terms of an arbitrarily positioned and oriented quadrupole coordinate system. Each Lagrangian cell or point is characterized by not only the hydrodynamic properties but also a set of chemistry quantities. The chemistry is loosely coupled to the hydrodynamics. Herein are presented details of the quadrupole coordinate system, the working form of the hydrodynamic equations and their initialization and methods for solution, the results of a test problem for a large-yield event at 200-km altitude producing motion in a linear array of six columns. (Author)

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Document Details

Document Type
Technical Report
Publication Date
Aug 08, 1975
Accession Number
ADA043546

Entities

People

  • Curtis A. Smith
  • Daniel A. Hamlin
  • Jon Y. Wang
  • Melvin R. Schoonover

Tags

Communities of Interest

  • C4I
  • Energy and Power Technologies
  • Weapons Technologies

DTIC Thesaurus Topics

  • Altitude
  • Arrays
  • Atmospheric Heave
  • Chemistry
  • Coordinate Systems
  • Difference Equations
  • Differential Equations
  • Electrons
  • Equations
  • Geometry
  • Grids
  • High Altitude
  • Hydrodynamics
  • Longitude
  • Plastic Explosives
  • Three Dimensional
  • Two Dimensional

Readers

  • Computer Science.
  • Finite Element Method (FEM) for solving Partial Differential Equations (PDEs)
  • Plasma Physics / Magnetohydrodynamics