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https://doi.org/10.1016/s1464-1917(00)00074-x
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Cite Publication Date: Jan 1, 2000 | |
 Citations: 5 |
Abstract Using N 2 measurements of the ESRO 4 satellite, the temperature increase in the polar thermosphere produced by the solar wind — magnetospheric energy source is investigated. It is demonstrated that this increase depends on local time and season.
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