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Influence of the B x component of the interplanetary magnetic field on magnetopause reconnection
Author(s) -
Gonzalez W. D.,
Gonzalez A. L. C.
Publication year - 1980
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/gl007i010p00773
Subject(s) - magnetopause , interplanetary magnetic field , physics , solar wind , electric field , polar , geophysics , magnetosphere , ionosphere , magnetic reconnection , convection , computational physics , astrophysics , magnetic field , mechanics , astronomy , quantum mechanics
A first clear evidence of an effect of the B x component (in Solar Magnetospheric Coordinates) of the Interplanetary Magnetic Field (IMF) on magnetopause reconnection has been obtained from polar ionospheric electric fields measured with balloons during an away sector of the IMF. This B x ‐ effect is such that larger electric field values were measured when B x was small, and vice versa, during intervals of time with B z ≤ O, and while the transverse component of the IMF and the solar wind speed had approximately constant values. For those cases, changes of B x form 2 to 8 gammas are found to account for as much as a factor of two decrease in the magnitude of the convection electric field at the polar cap. When B z > O, there is also some indication that the measured dusk to dawn polar cap electric field (reversed convection) became larger when |B x | was small and vice versa.