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GEOPHYSICAL RESEARCH LETTERS,
VOL. 31,
L08809,
doi:10.1029/2004GL020082,
2004
Stormtime observations of the flux of plasmaspheric ions to the dayside cusp/magnetopause
J. C. Foster
MIT Haystack Observatory, Westford, Massachusetts, USA
A. J. Coster
MIT Haystack Observatory, Westford, Massachusetts, USA
P. J. Erickson
MIT Haystack Observatory, Westford, Massachusetts, USA
F. J. Rich
Air Force Research Laboratory, Hanscom Air Force Base, Massachusetts, USA
B. R. Sandel
Lunar and Planetary Laboratory, University of Arizona, Tucson, Arizona, USA
Abstract
For the large geomagnetic disturbance on April 11, 2001, we combine data from the Millstone Hill radar, a network of GPS TEC
receivers, and the DMSP F-12 and IMAGE satellites, to estimate the sunward flux of thermal plasma associated with erosion
of the outer plasmasphere/ionosphere in the dusk sector. Direct radar observations of the E × B advection of SED plasma determine a flux of >10E26 ions/s to the noontime cusp at F-region heights. DMSP in situ observations provide a similar estimate. Assuming a dipolar magnetic field, we project our low-altitude
observations into the outer plasmasphere, obtaining a total sunward flux of >10E27 ions/s. High-altitude IMAGE EUV observations
of the plasmasphere drainage plume provides an estimate of 1.5 × 10E27 ions/s for the sunward flux. Such rates of sunward
plasma transport are sufficient to deplete a 1-Re shell of the outer plasmasphere in ∼1 hour.
Received 25
March
2004;
accepted 30
March
2004;
published 23
April
2004.
Index Terms: 2730 Magnetospheric Physics: Magnetosphere—inner; 2740 Magnetospheric Physics: Magnetospheric configuration and dynamics; 2760 Magnetospheric Physics: Plasma convection; 2768 Magnetospheric Physics: Plasmasphere; 2788 Magnetospheric Physics: Storms and substorms.
Read Full Article (file size: 945498 bytes) Cited by
Citation: Foster, J. C., A. J. Coster, P. J. Erickson, F. J. Rich, and B. R. Sandel
(2004),
Stormtime observations of the flux of plasmaspheric ions to the dayside cusp/magnetopause,
Geophys. Res. Lett.,
31,
L08809,
doi:10.1029/2004GL020082.
Copyright 2004 by the American Geophysical Union.
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