T. Ogawa et al., Plasma density suppression process around the cusp revealed by simultaneous CUTLASS and EISCAT Svalbard radar observations, J GEO R-S P, 106(A4), 2001, pp. 5551-5564
Simultaneous CUTLASS and EISCAT Svalbard radar (ESR) observations on Februa
ry 1, 1998, are used to study the generation of plasma density suppression,
which may ultimately result in polar cap patch formation, occurring: aroun
d the cusp region under IMF B, negative and By positive conditions. The CUT
LASS HF radars in Iceland and Finland observed F region plasma drifts in a
wide area including the ESR field of view while the ESR monitored electron
density, electron temperature, ion temperature, and ion motion along the ge
omagnetic field. We focus on two events for which the density suppressions
(30-60%) formed in harmony with strong plasma drifts (> 1500 ms(-1)) lastin
g for 5-12 min. In one-event, the suppression is mainly caused by enhanced
chemical reactions in the F region due to the intensified convection flows
which also raise ion temperature by 1500-2000 K through frictional heating.
This process can chop preexisting high-density region produced by energeti
c particle precipitation, maybe giving rise to polar patches. In the other
event, the density suppression is related to an appearance of eastward dire
cted high-speed plasma jets in a limited region with a latitudinal width of
> 100 km and a longitudinal extension of > 500 km. The ESR data, however,
show no ion temperature increase, suggesting that the suppression may not b
e caused by enhanced chemical reactions. We tentatively propose that the ea
stward plasma jets transported less dense plasma from earlier local times o
ver the ESR. Rapid change of IMF By polarity is another candidate for produ
cing the density suppression. A role of HF radar wave refraction in explain
ing this event is discussed.