Equatorial Plasma Instabilities and Mesospheric Turbulence - The Earth's Ionosphere: Plasma Physics and Electrodynamics - page 213

Bowles, K. L., Cohen, R., Ochs, G. R., and Balsley, B. B. (1960). Radar echoes from
field-aligned ionization above the magnetic equator and their resemblance to auroral
echoes. J. Geophys. Res . 65 , 1853.
Buneman, O. (1963). Excitation of field-aligned sound waves by electron streams. Phys.
Rev . Lett . 10 , 285.
Burke, W. J., Gentile, L. C., Huang, C. Y., Valladares, C. E., and Su, S.-Y. (2004). Longi-
tudinal variability of equatorial plasma bubbles observed by DMSP and ROCSAT-1.
J. Geophys. Res. 109 , A12301, doi:10.1029/2004JA010583.
Chau, J. L., and Woodman, R. F. (2001). Interferometric and dual beam observations
of daytime spread-F-like irregularities over Jicamarca. Geophys. Res. Lett . 28 (18),
3581.
Cho, J. Y. N., and Kelley, M. C. (1993). Polar mesosphere summer radar echoes: Obser-
vations and current theories. Rev. Geophys. 31 , 243.
Cohen, R., and Bowles, K. L. (1967). Secondary irregularities in the equatorial electrojet.
J. Geophys. Res . 72 , 885.
de La Beaujardiére, O., Retterer, J. M., Kelley, M. C., Hunton, D., and Jeong, L. (2006).
New satellite will forecast ionospheric disturbances. Space Weather 4 , S03C05,
10.1029/2005SW000145.
Dimant, Y. S. (2000). Nonlinearly saturated dynamical state of a three-wave mode-
coupled dissipative system with linear instability. Phys. Rev. Lett . 84 , 622.
Dimant, Y. S., and Sudan, R. N. (1997). Physical nature of new cross-field instability in
the lower ionosphere. J. Geophys. Res. 102 , 2551-2563.
Dungey, J. W. (1956). Convective diffusion in the equatorial F-region. J. Atmos. Terr.
Phys . 9 , 304.
Farley, D. T. (1963). A plasma instability resulting in field-aligned irregularities in the
ionosphere. J. Geophys. Res . 68 , 6083.
———. (1985). Theory of equatorial electrojet plasma waves: New developments and
current status. J. Atmos. Terr. Phys . 47 , 729.
Farley, D. T., and Hysell, D. L. (1996). Radar measurements of very small aspect angles
in the equatorial ionosphere. J. Geophys. Res . 101 , 5177.
Farley, D. T., and Providakes, J. F. (1989). The variation with T e and T i of the velocity
of unstable ionospheric two-stream waves. J. Geophys. Res. 94 , 15,415.
Farley, D. T., Balsley, B. B., Woodman, R. F., and McClure, J. P. (1970). Equatorial
spread F: Implications of VHF radar observations. J. Geophys. Res. 75 , 7199.
Fejer, B. G., and Kelley, M. C. (1980). Ionospheric irregularities. Rev. Geophys. Space
Phys . 18 , 401.
Fejer, B. G., Scherliess, L., and de Paula, E. R. (1999). Effects of the vertical plasma drift
velocity on the generation and evolution of equatorial spread F. J. Geophys. Res .
104 , 19,859.
Fejer, B. G., Farley, D. T., Baisley, B. B., and Woodman, R. F. (1975). Vertical structure
of the VHF backscattering region in the equatorial electrojet and the gradient drift
instability. J. Geophys. Res . 80 , 1313.
Gupta, S. P. (1986). Formation of sporadic E layers at low magnetic latitudes. Planet.
Space Sci . 34 , 1081.
Hagan, M. E., and Forbes, J. M. (2002). Migrating and nonmigrating diurnal tides in the
middle and upper atmosphere excited by tropospheric latent heat release. J. Geophys.
Res. 107 (D24), 4754, doi:10.1029/2001JD001236.