Physics
Scientific paper
Sep 1962
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1962jatp...24..805k&link_type=abstract
Journal of Atmospheric and Terrestrial Physics, vol. 24, no. 9, pp. 805-811
Physics
8
Scientific paper
The mathematical form of the diffusion operator is derived for motion of electrons along the lines of force of a dipole approximation to the geomagnetic field. The earth's atmosphere is assumed to be isothermal and horizontally stratified. A table is given of the various forms of the diffusion operator in different independent coordinates. The results are applied briefly to a discussion of the form of the boundary condition at great height in the F2-region.
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