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U.S. Department of Energy
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Plasma transport through the dayside cleft: A source of ionization patches in the polar cap

Technical Report ·
OSTI ID:7253441
Rapid sunward convection from the post-noon ionosphere carries high-density solar-produced F-region plasma through the dayside cleft and into the polar cap. This plasma is swept through the noontime cleft and enters the polar cap as a tongue of ionization which delineates the convection trajectory and its dynamics and provides the source for enhanced F-region plasmas and their effects which are observed at high polar latitudes away from noon.
Research Organization:
Massachusetts Inst. of Tech., Cambridge, MA (USA)
OSTI ID:
7253441
Report Number(s):
AD-A-214461/6/XAB
Country of Publication:
United States
Language:
English