High-latitude plasma outflow as measured by the DMSP spacecraft

Physics

Scientific paper

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Ionosphere: Ionosphere/Magnetosphere Interactions (2736), Ionosphere: Ionospheric Dynamics, Ionosphere: Auroral Ionosphere (2704), Ionosphere: Polar Cap Ionosphere, Ionosphere: Topside Ionosphere

Scientific paper

We have examined the vertical ion flux in the topside high-latitude ionosphere from measurements of the vertical ion drift and ion number density made by the DMSP F13 satellite. We found that the average vertical flux over the entire high-latitude region near 800 km altitude is quite small. This suggests that most of the vertical ion flux is associated with a large-scale ``breathing'' of the upper ionosphere. In the polar cap the vertical ion flux is uniformly downward at all locations. However, in the auroral zone the ion flux is highly structured, and a net upward flux is produced only by spatially and temporally confined events containing upward fluxes in excess of 1010 cm-2 s-1 that have no downward counterparts.

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