The effect of the atmosphere and ionosphere on long period magnetospheric micropulsations

Computer Science

Scientific paper

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Atmospheric Attenuation, Geomagnetic Micropulsations, Ionospheric Propagation, Magnetohydrodynamic Waves, Boundary Conditions, Boundary Value Problems, Earth Magnetosphere, Lines Of Force, Transverse Waves

Scientific paper

A study is made of the screening effect of the atmosphere and ionosphere which lets only part of a magnetospheric micropulsation signal reach the ground. Analytical expressions are obtained which relate the magnetic field in the magnetosphere to that on the ground; these expressions are confirmed by computing a full solution. Only the part of the signal with no vertical current will be seen on the ground; this agrees with previous work. Using this result, it is found that the reflection condition of a transverse hydromagnetic wave incident on the top of the ionosphere indicates a 'fixed-end' boundary condition for the field line. To a first approximation, micropulsation polarizations observed on the ground must be rotated through a right angle to obtain those in the magnetosphere. The strength of the electric field predicted in the ionosphere agrees with radio aurorae observations.

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