Cold ion heating at the dayside magnetopause during magnetic reconnection
Abstract Cold ions of ionospheric origin are known to be present in the magnetospheric side of the Earth's magnetopause. They can be very abundant, with densities up to 100 cm−3. These cold ions can mass load the magnetosphere, changing global parameters of magnetic reconnection, like the Alfvén spe...
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| Hlavní autoři: | , , , , , , , |
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| Médium: | Artigo |
| Jazyk: | Inglês |
| Vydáno: |
Wiley
2016-01-01
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| Edice: | Geophysical Research Letters |
| Témata: | |
| On-line přístup: | https://doi.org/10.1002/2015GL067187 |
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