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dc.contributor.authorLemaire, J.
dc.date1977
dc.date.accessioned2019-04-19T09:41:18Z
dc.date.available2019-04-19T09:41:18Z
dc.identifier.urihttps://orfeo.belnet.be/handle/internal/7226
dc.descriptionAssuming that the solar wind plasma is usually non-uniform over distances of 10,000 km or less, it is shown that filamentary plasma elements stretched out from the Sun can penetrate impulsively and become engulfed into the magnetosphere. The diamagnetic effects associated with these plasma inhomogeneities are observed in outer magnetospheres and magnetosheaths as dips or directional discontinuities in the magnetic field measurements. From the mean penetration distances of these diamagnetic plasma elements one can deduce a mean deceleration time, as well as an approximate value of the integrated Pedersen conductivity in the polar cusp of the Earth and Jupiter.
dc.languageeng
dc.titleImpulsive penetration of filamentary plasma elements into the magnetospheres of the Earth and Jupiter
dc.typeArticle
dc.subject.frascatiPhysical sciences
dc.audienceScientific
dc.source.titlePlanetary and Space Science
dc.source.volume25
dc.source.issue9
dc.source.page887-890
Orfeo.peerreviewedYes
dc.identifier.doi10.1016/0032-0633(77)90042-3


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