Date: Thursday, April 3, 2003
Time: 3:15 pm
Location: Packard 101
Special University Ph.D. Oral Examination
Global Dynamics of the Earth's Plasmasphere
Maria Spasojevic Department
of Electrical Engineering, Stanford University
Abstract
The plasmasphere is a region of cold (less than ~ 1 - 2 eV), dense
(~ 10 - 10^4 electrons cm^-3), plasma that encircles the Earth and
extends to geocentric equatorial distances ranging from ~ 2 to 7
Earth radii (RE). At the outer boundary of the plasmasphere, there
typically exists a sharp gradient in the equatorial electron density
profile known as the plasmapause. The size and shape of the
plasmasphere vary considerably due to recurring geomagnetic
storm and substorm activity.
The plasmasphere erosion and recovery processes have been
studied but only from the relatively limited perspective of
individual (or, occasionally, multiple) ground stations and satellite
crossings of the plasmapause and plasmasphere. The global-scale,
multi-hour images of the plasmasphere now available from the
Extreme Ultraviolet Imager (EUV) of the IMAGE mission allow
us to address ongoing and fundamental questions about the
structure and dynamics of the plasmasphere system.
The EUV instrument images the He+ distribution in the Earth's
plasmasphere by detecting resonantly scattered solar 30.4-nm
radiation and produces images with ~ 0.1 RE spatial resolution
every 10 minutes. Tracking the location of the plasmapause in
sequences of EUV images allows quantitative measurements of
radial and azimuthal motions of the boundary during various
phases of geomagnetic disturbances. Specifically, we show inward
motions and steepening of the plasmapause boundary on the
nightside of the Earth, the formation and evolution of
plasmaspheric drainage plumes, and the tendency for the
development of mesoscale azimuthal irregularities in the
plasmapause radius in a specific local time sector. In addition, we
calculate the total amount of He+ (and thus infer the total amount
of plasma) removed from the plasmasphere during specific periods
of enhanced geomagnetic activity.
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