Computer Science
Scientific paper
Mar 1978
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1978p%26ss...26..201n&link_type=abstract
Planetary and Space Science, vol. 26, Mar. 1978, p. 201-209.
Computer Science
36
Damping, Geomagnetic Pulsations, Ionospheric Conductivity, Magnetohydrodynamic Waves, Wave Attenuation, Earth Magnetosphere, Harmonic Oscillation, Transverse Waves, Wave Equations
Scientific paper
The damping of low frequency transverse hydromagnetic waves by the ionosphere is investigated by computing the damping experienced by standing Alfven waves in a dipole magnetic field. Both the uncoupled poloidal and toroidal modes are considered with Joule dissipation being introduced through a boundary condition which relates the electric and magnetic field strengths at the ionosphere. Numerical calculations are restricted to the field line resonance region, and the signal is assumed to be purely transverse. Damping rates are strongly dependent on ionospheric conductivity; typically, the normalized damping rate is found to be approximately 0.1 for nightside values of conductivity and approximately 0.01 for the dayside. It is suggested that this circumstance would account for the observed scale of bandwidths in pulsation signals.
Hughes Jeffrey W.
Newton R. S.
Southwood David J.
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