Unsolved problems in plasmasphere refilling
Autor: | Dennis L. Gallagher, R. H. Comfort |
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Rok vydání: | 2016 |
Předmět: |
010504 meteorology & atmospheric sciences
Magnetosphere Plasmasphere Context (language use) Plasma Geophysics 01 natural sciences Physics::Geophysics Magnetic field Magnetosheath Space and Planetary Science Physics::Space Physics 0103 physical sciences Outflow Astrophysics::Earth and Planetary Astrophysics Ionosphere 010303 astronomy & astrophysics Geology 0105 earth and related environmental sciences |
Zdroj: | Journal of Geophysical Research: Space Physics. 121:1447-1451 |
ISSN: | 2169-9402 2169-9380 |
DOI: | 10.1002/2015ja022279 |
Popis: | The plasmasphere is a cold (~1 eV) plasma at middle to low magnetic latitudes surrounding the Earth. Its shape is dominated by Earth's magnetic field and its cross-field motion is dominated by electric fields. It is a highly coupled part of the inner magnetosphere. Storm time conditions erode the outer plasmasphere, transporting that plasma into the dayside magnetosheath region, leaving behind a region of greatly reduced plasma density that will refill from ionospheric outflow. The processes involved in refilling remain incompletely understood. In this commentary, outstanding questions about plasmaspheric refilling are summarized in the context of recent publications. |
Databáze: | OpenAIRE |
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