Ionospheric O + Momentum Balance Through Charge Exchange With Thermospheric O Atoms
نویسندگان
چکیده
منابع مشابه
Ionospheric origin of magnetospheric O+ ions
Flows of thermal atomic oxygen (0 +) ions are deduced from topside ionospheric plasma density profiles. The mean flux within most of the polar cap is of the order of lO 12 m -2 s-l, a figure which is consistent with both theoretical and experimental estimates of the light ion at . polar wind eater altitudes Larger flows (up to 6 x lOl•m-2s-1) are observed n ar the poleward edge of the night-sid...
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ژورنال
عنوان ژورنال: Journal of Geophysical Research: Space Physics
سال: 2018
ISSN: 2169-9380,2169-9402
DOI: 10.1029/2018ja025821