Astronomy and Astrophysics – Astronomy
Scientific paper
Nov 1996
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1996babel.154...29g&link_type=abstract
Bulletin Astronomique de Belgrade No. 154, page 29-34 (1996).
Astronomy and Astrophysics
Astronomy
Scientific paper
The current density in the dynamo region is estimated from thermospheric neutral wind pattern and plasmaspheric electric field. The diurnal variation of the meridional and the zonal component of the neutral wind velocity, is established from the altitudes of the descending sporadic E layer. The diurnal change of the westward electric field that maps from the dynamo region into the plasmasphere is deduced from the whistler data The vertical ionosonde data on sporadic E heights, h'Es, taken at Grocka observatory (44.6^{\circ}N, 20.8^{\circ}E), are used. The selected whistlers were recorded at Grocka station (L ~1.9). All ground-base data used in this study were registered on quiet days.
Grubor D. P.
Šulić D. M.
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