Geoscience Reference
In-Depth Information
———. (2004b). Coupling of the Perkins instability and the sporadic E layer
instability derived from physical arguments. J. Geophys. Res . 109 , A06301,
doi:10.1029/2003JA010295.
Cox, R. M. and Plane, J. M. C. (1998). An ion-molecule mechanism for the formation of
neutral sporadic Na layers. J. Geophys. Res. 103 , 6349-6360.
Dimant, Y. S., and Oppenheim, M. M. (2004). Ion thermal effects on E-region
instabilities: Linear Theory. J. Atmos. Solar-Terr. Phys. 66 (17), 1639-1654,
doi:10.1016/j.jastp.2004.07.006.
Dimant, Y. S., and Sudan, R. N. (1995). Kinetic theory of low-frequency cross-field
instability in a weakly ionized plasma, 1. Phys. Plasma 2 (4), 1157-1168.
Djuth, F., Sulzer, M., Elder, J., and Wickwar, V. (1997). High-resolution studies of
atmosphere-ionosphere coupling at Arecibo Observatory, Puerto Rico. Radio Sci .
32 (6), 2321-2344.
Drummond, J. D., Grime, B. W., Gardner, C. S., Liu, A., Chu, X., Kelley, M. C., and
Kane, T. J. (2001). Observations of persistent Leonid meteor trails: 1. Advection of
the “Diamond Ring.” J. Geophys. Res . 106 (A10), 21, 517-21, 524.
Dungey, J. W. (1959). Effect of a neutral field turbulence in an ionized gas. J. Geophys.
Res. 64 , 2188.
Eckart, C. (1960). Hydrodynamics of Oceans and Atmospheres . Pergamon Press, NY.
England, S. L., Maus, S., Immel, T. J., and Mende, S. B. (2006). Longitudinal variation
of the E-region electric fields caused by atmospheric tides. Geophys. Res. Lett . 33 ,
L21105, doi:10.1029/2006GL027465.
Farley, D. T. (1959). A theory of electrostatic fields in a horizontally stratified ionosphere
subject to a vertical magnetic field. J. Geophys. Res . 64 , 1225.
———. (1960). A theory of electrostatic fields in the ionosphere at nonpolar geomagnetic
latitudes. J. Geophys. Res . 65 , 869-877.
Foster, J. C., Erickson, P. J., Coster, A. J., Goldstein, J., and Rich, F. J. (2002).
Ionospheric signatures of plasmaspheric tails. Geophys. Res. Lett. 29 (13),
doi:10.1029/2002GL015067.
Francis, S. H., and Perkins, F. W. (1975). Determination of striation scale sizes for plasma
clouds in the ionosphere. J. Geophys. Res. 80 , 3111.
Fukao, S., Kelley, M. C., Shirakawa, T., Takami, T., Yamamoto, M., Tsuda, T., and Kato,
S. (1991). Turbulence upwelling of the midlatitude ionosphere, 1. Observational
results by the MU radar. J. Geophys. Res . 96 , 3725-3746.
Fukao, S., Sato, T., Tsuda, T., Yamamoto, M., Yamanaka, M. D., and Kato, S. (1990).
The MU radar: New capabilities and system calibrations. Radio Sci . 25 , 477.
Fukao, S., Yamamoto, M., Tsunoda, R., Hayakawa, H., and Mukai, T. (1998). The
SEEK (Sporadic-E Experiment over Kyushu) campaign. Geophys. Res. Lett . 25 (11),
1761-1764.
Garcia, F. J., Kelley, M. C., Makela, J. J., and Huang, C.-S. (2000a). Airglow observa-
tions of mesoscale low-velocity traveling ionospheric disturbances at midlatitudes.
J. Geophys. Res . 105 (A8), 18, 407-18, 415.
Garcia, F. J., Kelley, M. C., Makela, J. J., Sultan, P. J., Pi, X., and Musman, S. (2000b).
Mesoscale structure of the midlatitude ionosphere during high geomagnetic activity:
Airglow and GPS observations. J. Geophys. Res . 105 (A8), 18, 417-18, 427.
Gershman, B. N. (1974). Dynamics of Ionospheric Plasma . Nauka, Moscow.
Search WWH ::




Custom Search