skip to main content
OSTI.GOV title logo U.S. Department of Energy
Office of Scientific and Technical Information

Title: Lunar tidal variations in the equatorial electrojet current

Journal Article · · Journal of Geophysical Research

The lunar semidiurnal variations in the solar diurnal range of the horizontal component of the earth' s magnetic field H are computed for the equatorial stations that were operating in Peru during the IGY and IGC. The amplitude is found to be greatly enhanced on either side of the magnetic equator within magnetic dip of about 450 deg C in a 10 un. Concent 85% . The narrow regions of enhanced lunar tidal effect and solar diurnal variation in H are similar to each other, suggesting that lunar semidiurnal tides affect the same region as that containing the well-known solar diurnal equatorial electrojet. The lunar effects in South America are found to be maximum during the southern solstice at stations within the zone of the equatorial electrojet, but during the equinoxes at stations in middle latitudes.

Research Organization:
Physical Research Lab., Ahmedabad, India
Sponsoring Organization:
USDOE
NSA Number:
NSA-17-023514
OSTI ID:
4723784
Journal Information:
Journal of Geophysical Research, Vol. 68, Issue 9; Other Information: Orig. Receipt Date: 31-DEC-63; ISSN 0148-0227
Publisher:
American Geophysical Union
Country of Publication:
Country unknown/Code not available
Language:
English

Similar Records

Recent measurements of the magnetic field of the equatorial electrojet in Nigeria
Journal Article · Wed May 01 00:00:00 EDT 1963 · Journal of Geophysical Research · OSTI ID:4723784

Variability of the equatorial electrojet: Its relations to the Sq current system and semidiurnal tides
Journal Article · Fri Nov 01 00:00:00 EST 1991 · Geophysical Research Letters (American Geophysical Union); (United States) · OSTI ID:4723784

Solar tides in the equatorial upper thermosphere: A comparison between AE-E data and the TIGCM for solstice, solar minimum conditions
Journal Article · Tue Jan 01 00:00:00 EST 1991 · Journal of Geophysical Research; (United States) · OSTI ID:4723784