Velocity boundary layers in the distant geotail and the Kelvin Helmholtz instability

Physics

Scientific paper

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Scientific paper

The formation of velocity boundary layers at the flanks of the distant
geotail due to the Kelvin Helmholtz instability has been studied. It is
shown that the build-up of slow oblique perturbations leads to an
anomalous viscosity sufficient for the formation of thick boundary
layers in the distant magnetotail.

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