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IMF b/sub y/ control of ionization and electric fields measured by the Sondrestrom radar

Technical Report ·
OSTI ID:6512030
The pattern of ionization and electric fields measured in the dayside auroral zone by the Sondrestrom incoherent scatter radar is compared with interplanetary magnetic field (IMF) data from the IMP-8 spacecraft. The electric-field configuration is most sensitive to the B/sub y/ component of the IMF. For B/sub y/ < 0 there is a strong reversal in convective flow between 1300 and 1600 MLT with a region of enhanced F-region ionization associated with low-energy particle precipitation at the reversal. For B/sub y/ > 0 the convention reversal is most apparent on the morning side. Ionization produced by particle precipitation for B/sub y/ > 0. is much less conspicuous than that observed on the afternoon side for B/sub y/ <0. We show radar measurements of ionization, electric fields and electron temperatures associated with two distinct types of particle precipitation in the pre-noon local time sector for B/sub y/> 0. The patterns of precipitation for B/sub y/ < 0 and B/sub y/ > 0 are consistent with the distribution of field-aligned currents, in that precipitation occurs primarily in the upward current regions. With this interpretation, only the precipitation associated with the cusp-field-aligned currents on the dawn side may be intense enough to produce ionospheric signatures observable from the ground.
Research Organization:
Stanford Univ., CA (USA). Space, Telecommunications and Radioscience Lab.
OSTI ID:
6512030
Report Number(s):
AD-A-177814/1/XAB
Country of Publication:
United States
Language:
English