Enhanced velocities and a shear in daytimeEsqover Kwajalein and their relationship to 150 km echoes over the dip equator
Author:
Publisher
American Geophysical Union (AGU)
Subject
General Earth and Planetary Sciences,Geophysics
Link
http://www.agu.org/journals/gl/v021/i024/94GL02507/94GL02507.pdf
Reference14 articles.
1. The wind-shear theory of temperate zone sporadic E;Axford;Radio Sci.,1966
2. Evidence of a stratified echoing region at 150 km in the vicinity of the magnetic equator during daylight hours;Balsley;J. Geophys. Res.,1964
3. Some characteristics of non-two-stream irregularities in the equatorial electrojet;Balsley;J. Geophys. Res.,1969
4. On the plasma instability mechanisms responsible for Esq;Balsley;J. Geophys. Res.,1976
5. Some aspects of Es ionization of the magnetic equatorial region;Bandyopadhyay;J. Geophys. Res.,1963
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