Equatorial Plasma Instabilities and Mesospheric Turbulence - The Earth's Ionosphere: Plasma Physics and Electrodynamics - page 218

Sekar, R., and Raghavarao, R. (1987). Role of vertical winds on the Rayleigh-Taylor
instabilities of the nighttime equatorial ionosphere. J. Atmos. Terr. Phys. 49 , 981.
Shume, E. B., Hysell, D. L., and Chau, J. L. (2005). Zonal wind velocity profiles in the
equatorial electrojet derived from phase velocities of type II radar echoes. J. Geophys.
Res . 110 , 12,308.
Simon, A. (1963). Instability of a partially ionized plasma in crossed electric and magnetic
fields. Phys. Fluids 6 , 382.
Sridharan, R., Pallam Raju, D., Raghavarao, R., and Ramarao, P. V. S. (1994). Precursor
to equatorial spread-F in O I 630.0 nm dayglow. Geophys. Res. Lett. 21 , 2797.
Sridharan, R., Chandra, H., Das, S. R., Sekar, R., Sinha, H. S. S., Pallam Raju, D.,
Narayanan, R., Raizada, S., Misra, R. N., Raghavarao, R., Vyas, G. D., Rao, P. B.,
Ramarao, P. V. S., Somayajulu, V. V., Babu, V. V., and Danilov, A. D. (1997).
Ionization Hole Campaign—A coordinated rocket and ground-based study at the
onset of equatorial spread F: First results. J. Atmos. Terr. Phys. 59 , 2051.
St.-Maurice, J.-P., and Kissack, R. S. (2000). The role played by thermal feedbacks in
heated Farley-Buneman waves at high latitudes. Ann. Geophys. 18 , 532-548.
St.-Maurice, J.-P., Choudhary, R. K., Ecklund, W. L., and Tsunoda, R. T. (2003).
Fast type-I waves in the equatorial electrojet: Evidence for non-isothermal
ion-acoustic speeds in the lower E region. J. Geophys. Res. 108 (5), 1170,
doi:10.1029/2002JA009648.
Sudan, R. N. (1983). Unified theory of type 1 and type 2 irregularities in the equatorial
electrojet. J. Geophys. Res . 88 , 4853.
Sudan, R. N., and Keskinen, M. (1977). Theory of strongly turbulent two-dimensional
convention of low pressure plasma. Phys. Rev. Lett . 38 , 966.
Sudan, R. N., Akinrimisi, J., and Farley, D. T. (1973). Generation of small-scale irregu-
larities in the equatorial electrojet. J. Geophys. Res . 78 , 240.
Swartz, W. E. (1997). CUPRI observations of persistence asymmetry reversals in up-
down vertical type-I echoes from the equatorial electrojet above Alcântara, Brazil.
Geophys. Res. Lett. 24 (13), 1675-1678.
Tatarskii, V. I. (1971). The Effects of the Turbulent Atmosphere on Wave Propagation .
Israel Program for Scientific Translations, Jerusalem.
Tennekes, H., and Lumley, J. L. (1972). A First Course in Turbulence , MIT Press,
Cambridge.
Tsunoda, R. T. (1981). Time evolution and dynamics of equatorial backscatter plumes.
1. Growth phase. J. Geophys. Res . 86 , 139.
———. (1983). On the generation and growth of equatorial backscatter plumes. 2. Struc-
turing of the west walls of upwellings. J. Geophys. Res . 88 , 4869.
———. (1985). Control of the seasonal and longitudinal occurrence of equatorial scin-
tillations by the longitudinal gradient in integrated E-region Pedersen conductivity.
J. Geophys. Res. 90 , 447.
Tsunoda, R. T., Livingston, R. C., McClure, J. P., and Hanson, W. B. (1982). Equa-
torial plasma bubbles: Vertically elongated wedges from the bottomside F layer.
J. Geophys. Res . 87 , 9171.
Varney, R. H., Kelley, M. C., and Kudeki, E. (2009). Observations of electric
fields associated with internal gravity waves. J. Geophys. Res . 114 , A02304,
doi:10.1029/2008JA013733.
Whitehead, J. D. (1971). Ionization disturbances caused by gravity waves in the presence
of an electrostatic field and background wind. J. Geophys. Res. 76 , 238.