Effects of Diffusion of Electrons near the Magnetic Equator

IN a recent interesting communication, Dr. E. R. Schmerling 1 has discussed the possible effect of vertical diffusion in the ionosphere in the presence of the geomagnetic field. He claims that the effect of diffusion is to increase the electron density below the electron peak, so that near the magne...

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Veröffentlicht in:Nature 1960-12, Vol.188 (4755), p.1017-1018
Hauptverfasser: FERRARO, V. C. A., GLIDDON, J. E. C., KENDALL, P. C.
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GLIDDON, J. E. C.
KENDALL, P. C.
description IN a recent interesting communication, Dr. E. R. Schmerling 1 has discussed the possible effect of vertical diffusion in the ionosphere in the presence of the geomagnetic field. He claims that the effect of diffusion is to increase the electron density below the electron peak, so that near the magnetic equator the electron density N at a given height h should be less than in slightly higher latitudes, since the magnetic field at the equator is horizontal and precludes vertical diffusion. Dr. Schmerling, however, assumes in this derivation that the rate of ion production is independent of latitude and therefore of the magnetic dip.
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subjects COSMIC RADIATION
DIFFUSION
EARTH
ELECTRONS
GEOMAGNETIC EQUATOR
Humanities and Social Sciences
IONIZATION
IONOSPHERE
IONS
LATITUDE EFFECT
letter
LEVELS
MAGNETIC FIELDS
multidisciplinary
PHYSICS
PRODUCTION
Science
Science (multidisciplinary)
VARIATIONS
ZONES
title Effects of Diffusion of Electrons near the Magnetic Equator
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