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Convection at high latitudes when the interplanetary magnetic field is northward
Authors:BV Rezhenov
Institution:Polar Geophysical Institute, Apatity 184200, U.S.S.R.
Abstract:It is shown that the pattern of convection at high latitudes when the IMF is northward is the sum of two types of convection: (a) four-vortex convection completely closed in high latitudes and (b) homogeneous sunward convection across all high-latitude regions including the auroral zone. The decay of the three-dimensional current system which existed before the turning of IMF northwards may maintain the homogeneous sunward convection.
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