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Title: AMPTE lithium tracer releases in the solar wind: Observations inside the magnetosphere

Journal Article · · J. Geophys. Res.; (United States)

A release of approximately 3.3 x 10/sup 25/ lithium atoms was made on September 11 and again on September 20, 1984, by the Active Magnetospheric Particle Tracer Explorers (AMPTE) Ion Release Module (IRM) spacecraft at a geocentric distance of roughly-equal18.8 R/sub e/ in the subsolar direction, creating an ion cloud approximately 4 R/sub e/ in diameter after one hour. Detailed modeling of ion propagation to the bow shock and transport through the magnetosheath shows that > or approx. =20% (September 11) and > or approx. =50% (September 20) of the ions mapped to a 36-R/sub e//sup 2/ area around the stagnation point on the magnetopause. The AMPTE Charge Composition Explorer (CCE) satellite, located inside the magnetosphere with an apogee of 8.78 R/sub e/ and inclination of 4.8/sup 0/, at a local time of about 1300 MLT, was instrumented to detect lithium ions over the energy range from a few eV to > or approx. =6 MeV. Detailed analysis of the data for the several hours following the lithium releases shows that no measurable lithium ion fluxes reached the location of the CCE; upper limits to the lithium flux at L> or approx. =8 are about 50 to 70 (cm/sup 2/-sec-sr)/sup -1/ in the range 25--300 keV/e (Li/H> or approx. =2 x 10/sup -5/), and about 0.1 to 1 (cm/sup 2/-sec-sr)/sup -1/ in the range 45--100 keV/nucleon (Li/Hroughly-equal1 x 10/sup -6/). The implications of these results are discussed in the context of current theoretical models of plasma entry into and transport within the magnetosphere.

Research Organization:
The Johns Hopkins University Applied Physics Laboratory, Laurel, Maryland
OSTI ID:
6101766
Journal Information:
J. Geophys. Res.; (United States), Vol. 91:A2
Country of Publication:
United States
Language:
English