ION DISTRIBUTION DYNAMICS NEAR THE EARTHS BOW SHOCK - FIRST MEASUREMENTS WITH THE 2D ION ENERGY SPECTROMETER CORALL ON THE INTERBALL TAIL-PROBE SATELLITE/
Yi. Yermolaev et al., ION DISTRIBUTION DYNAMICS NEAR THE EARTHS BOW SHOCK - FIRST MEASUREMENTS WITH THE 2D ION ENERGY SPECTROMETER CORALL ON THE INTERBALL TAIL-PROBE SATELLITE/, Annales geophysicae, 15(5), 1997, pp. 533-541
The dynamics of the ion distribution function near the Earth's bow sho
ck is studied on the basis of quasi-3D measurements of ion energy spec
tra in the range of 30-24200 eV/q with the Russian-Cuban CORALL instru
ment on the INTERBALL/Tail-probe satellite. The instrument was designe
d for observations of magnetospheric plasma and measures ions, in an a
ngular range of 36 degrees-144 degrees from the Earth-Sun direction. I
on populations generated by the Earth bow shock are often observed ups
tream from the bow shock. In the solar-wind stream compressed and heat
ed by the passing of very dense magnetic cloud (CME), two types of the
se ion populations were measured upstream and before the bow shock cro
ssing on 25 August 1995 at 07:37 UT. Both populations were observed in
the energy range above 2 keV. At similar to 06:20 UT, when the angle
between the direction of the interplanetary magnetic field and normal
to the bow shock upsilon(Bn) was similar or equal to 43 degrees the in
strument observed a narrow, fast (similar to 800 km/s) field-aligned b
eam moving from the Earth. At similar to 07:30, when upsilon(Bn) simil
ar or equal to 28 degrees, the wide ion pitch-angle distribution was o
bserved. A similar suprathermal ion population is observed in the magn
etosheath simultaneously with the solar-wind ion population being heat
ed and deflected from the Sun-Earth direction. The similarity of obser
vations during the mentioned time-interval and under usual solar-wind
conditions allows us to conclude that types of suprathermal ion popula
tions upstream and downstream from the bow shock do not depend on the
solar-wind disturbance generated by magnetic cloud.