The temporal and spatial variations of low frequency geomagnetic pulsations at polar cusp and cap latitudes

Geomagnetic field measurements at two Antarctic stations are compared during two weeks in the local summer (January 1-15, 1992). Low frequency (0.6-6 mHz) pulsations are observed at each station near local magnetic noon. The same wave packets appear in some cases also at the other station, although...

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Bibliographic Details
Main Authors: Kleimenova, N. G., Francia, P., Villante, U., Kozyreva, O. V., Bitterly, J., Schott, J. J.
Other Authors: Kleimenova, N. G.; Institute of the Physics of the Earth, Moscow, Russia, Francia, P.; Dipartimento di Fisica, Università dell'Aquila, Coppito, L'Aquila, Italy, Villante, U.; Dipartimento di Fisica, Università dell'Aquila, Coppito, L'Aquila, Italy, Kozyreva, O. V.; Institute of the Physics of the Earth, Moscow, Russia, Bitterly, J.; Institute de Physique du Globe, Chambon-la-Foret Observatoire, Paris, France, Schott, J. J.; Ecole et Observatoire des Sciences de la Terre, Strasbourg, France, Institute of the Physics of the Earth, Moscow, Russia, Dipartimento di Fisica, Università dell'Aquila, Coppito, L'Aquila, Italy, Institute de Physique du Globe, Chambon-la-Foret Observatoire, Paris, France, Ecole et Observatoire des Sciences de la Terre, Strasbourg, France
Format: Article in Journal/Newspaper
Language:English
Published: 1999
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Online Access:http://hdl.handle.net/2122/1403
Description
Summary:Geomagnetic field measurements at two Antarctic stations are compared during two weeks in the local summer (January 1-15, 1992). Low frequency (0.6-6 mHz) pulsations are observed at each station near local magnetic noon. The same wave packets appear in some cases also at the other station, although with a significant attenuation, more clearly in the morning sector; the waves show a near noon reversal of the polarization sense from counter-clockwise in the morning to clockwise in the afternoon indicating a westward and an eastward propagation, respectively. JCR Journal open