T. Mukai et al., THE LOW-ENERGY PARTICLE (LEP) EXPERIMENT ONBOARD THE GEOTAIL SATELLITE, Journal of Geomagnetism and Geoelectricity, 46(8), 1994, pp. 669-692
The low energy particle (LEP) instrument onboard GEOTAIL is designed t
o make comprehensive observations of plasma and energetic electrons an
d ions with fine temporal resolution in the terrestrial magnetosphere
(mainly magnetotail) and in the interplanetary medium. It consists of
three units of sensors (LEP-EA, LEP-SW and LEP-MS) and a common electr
onics (LEP-E). The Energy-per-charge Analyzers (EA) measure three-dime
nsional velocity distributions of electrons (with EA-e) and ions (with
EA-i), simultaneously and separately, over the energy-per-charge rang
e of several eV/q to 43 keV/q. Emphasis in the EA design is laid on th
e large geometrical factor to measure tenuous plasma in the magnetotai
l with sufficient counting statistics in the high-time-resolution meas
urement. On the other hand, the Solar Wind ion analyzer (SW) has small
er geometrical factor, but fine angular and energy resolutions, to mea
sure energy-per-charge spectra of the solar wind ions. In both EA and
SW sensors, the complete three-dimensional velocity distributions can
only be obtained in a period of four spins, while the velocity moments
up to the third order are calculated onboard every spin period (nomin
ally, 3 sec). The energetic-ion Mass Spectrometer (MS) can provide thr
ee-dimensional determinations of the ion composition. In this paper, w
e describe the instrumentation and present some examples of the inflig
ht measurements.