DE-1 observations of the polar wind-A heated and an unheated component
作者： C. Gurgiolo , J. L. Burch
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摘要: High altitude observations made by DE-1 in the polar regions indicate that wind consists of both a heated and an unheated component. The component constitutes what may be called “classical wind” while is thought to result interaction primal with ion perpendicular heating. at which heating occurs estimated lie between 8000 12000 km.
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