The yearly mean Disturbance Daily (SD) variation, i.e., solar daily variati
on on International Disturbed days (Sd) minus that on International Quiet d
ays (Sq) of the geomagnetic H field at Huancayo, an equatorial electrojet s
tation in American zone, for any of the years 1954-61 shows a dawn-maximum
and a dusk-minimum as observed at any low and middle latitude station. Cont
rary to this, the SD(H) variation at Kodaikanal, an equatorial station in t
he Indian zone, shows a prominent minimum around noon hours besides the usu
al dawn-maximum and dusk-minimum for any of these years. The amplitude of S
D(H) at Huancayo or at Kodaikanal decreases with the decreasing solar activ
ity. Seasonally, SD(H) is larger during equinoctial than during solsticial
months. For any particular season, the SD(H) averaged for all hours of the
day is lower at Huancayo than at Kodaikanal, while the Sq(H) at Huancayo is
always greater than the corresponding amplitude of Sq(H) at Kodaikanal. Th
us the sources of electrojet electric fields on quiet and on disturbed days
seem to be different and need to be identified. (C) 1998 Elsevier Science
Ltd. All rights reserved.