Rastogi, R. G. (1973) Equatorial sporadic-E and the electric field Journal of Atmospheric and Terrestrial Physics, 35 (2). 367-368, IN3, 369. ISSN 0021-9169
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Official URL: http://www.sciencedirect.com/science/article/pii/0...
Related URL: http://dx.doi.org/10.1016/0021-9169(73)90103-7
Abstract
It is shown that the q type of equatorial Es at Huancayo disappears during the daytime hours when the drifts measured by Doppler shift of VHF radar echoes indicate extremely small values or an eastward E-region or downward F-region drifts. The Es-q is suggested to be due to cross field irregularities and its disappearance is due to temporary reversal of the horizontal E-region electrostatic field causing reversal or the stoppage of equatorial electrojet currents.
Item Type: | Article |
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Source: | Copyright of this article belongs to Elsevier Science. |
ID Code: | 45910 |
Deposited On: | 29 Jun 2011 06:45 |
Last Modified: | 29 Jun 2011 06:45 |
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