Propagation of Hydrogentic waves in the upper F2-region>

Details Propagation of Hydrogentic waves in the upper F2-region> Propagation of Hydrogentic waves in the upper F2-region>

Dec 1973

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1973p%26ss...21.2157h&link_type=abstract

Planetary and Space Science, Volume 21, Issue 12, p. 2157-2171.

Physics

Scientific paper

The theory of hydromagnetic-wave in the upper F2-region, in which electrons are in a transitional regime from collisional to collisionless conditions and ions are in a collisionless state, is examined. Derivation of the governing equations is based on the fact that the isotropic electrons are fluid-like, and the anisotropic ions follow kinetic equations modified by ion-electron collisions. Magneto-acoustic waves of a period of ~0.2-10 sec are dissipated by ion Landau damping and electron thermal conduction and viscosity. Numerical solutions under ionospheric conditions show that the dissipation of hydromagnetic waves is insufficient to modify the large scale heating of the ionosphere.

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