dc.contributor.author |
Rastogi, R. G |
|
dc.date.accessioned |
2013-05-30T09:59:48Z |
|
dc.date.available |
2013-05-30T09:59:48Z |
|
dc.date.issued |
1975-04 |
|
dc.identifier.citation |
Geophysical Research Letters, Vol. 2, No. 4, pp. 142–145 |
en |
dc.identifier.issn |
0094-8276 |
|
dc.identifier.uri |
http://hdl.handle.net/2248/6073 |
|
dc.description |
Open Access |
en |
dc.description.abstract |
During geomagnetic disturbed periods, the q type of sporadic E layer near the dip equator is shown to disappear with maximum error of five minutes during the period when the difference of the geomagnetic H field between the equatorial and non-equatorial station decreases below the night level. These periods are identified with the reversal to westward direction of the electrojet currents at the base of the E region around 100 km level irrespective of the changes in the Sq current system which might be produced by the disturbance. |
en |
dc.language.iso |
en |
en |
dc.publisher |
The American Geophysical Union |
en |
dc.relation.uri |
http://dx.doi.org/10.1029/GL002i004p00142 |
en |
dc.rights |
© The American Geophysical Union. |
en |
dc.title |
Westward ionospheric currents over the dip equator during geomagnetic disturbances |
en |
dc.type |
Article |
en |