Waves and Instabilities at Midlatitudes - The Earth's Ionosphere: Plasma Physics and Electrodynamics - page 340

Saito, A., Iyemori, T., Sugiura, M., Maynard, N. C., Aggson, T., Brace, L. H., Takeda,
M., and Yamamoto, M. (1995). Conjugate occurrence of the electric field fluctua-
tions in the nighttime midlatitude Ionosphere. J. Geophys. Res. 100 , 21, 439-21,
451.
Saito, A., Nishimura, M., Yamamoto, M., Fukao, S., Kubota, M., Shiokawa, K.,
Otsuka, Y., Tsugawa, T., Ogawa, T., Ishii, M., Sakanoi, T., and Miyazaki, S. (2001).
Traveling ionospheric disturbances detected in the FRONT campaign. Geophys. Res.
Lett . 28 (4), 689-692, 10.1029/2000GL011884.
Schlegel, K., and Haldoupis, C. (1994). Observation of the modified two-stream plasma
instability in the midlatitude E region ionosphere. J. Geophys. Res . 99 , 6219.
Schutz, S., Adams, G. J., and Mozer, F. S. (1973). Probe electric field measurements near
a midlatitude ionospheric barium release. J. Geophys. Res . 78 , 6634.
Seyler, C. E., Rosado-Roman, J. M., and Farley, D. T. (2004). A nonlocal theory of the
gradient-drift instability in the ionospheric E region plasma at midlatitudes. J. Atmos.
Solar Terr. Phys. 66 , 1627-1637.
Shalimov, S., Haldoupis, C., and Schlegel, K. (1998). Large polarization electric fields
associated with midlatitude sporadic E. J. Geophys. Res . 103 , 11, 617.
Shalimov, S., andHaldoupis, C. (2005). E region wind-driven electrical coupling of patchy
sporadic E and spread F at midlatitude. Ann. Geophys . 23 , 2095-2105.
Shen, J. S., Swartz, W. E., Farley, D. T., and Harper, R. M. (1976). Ionization layers in
the nighttime E region valley above Arecibo. J. Geophys. Res . 81 , 5517.
Shiokawa, K., Otsuka, Y., Ihara, C., Ogawa, T., and Rich, F. J. (2003). Ground and
satellite observations of nighttime medium-scale traveling ionospheric disturbance
at midlatitude. J. Geophys. Res. 108 (A4), 1145, doi:10.1029/2002JA009, 639.
Sinno, K., Ouchi, C., Nemoto, C., and Futagawa, H. (1965). Structure and movement
of E s detected by LORAN observations (supplemental report). J. Radio Res. Lab .
12 , 59.
Smith, L. G., andMiller, K. L. (1980). Sporadic layers and unstable wind shears. J. Atmos.
Terr. Phys . 42 , 45.
Swartz, W. E., Collins, S. C., Kelley, M. C., Makela, J. J., Kudeki, E., Franke, S., Urbina, J.,
Aponte, N., González, S., Sulzer, M. P., and Friedman, J. S. (2002). First observations
of an F region turbulent upwelling coincident with severe E region plasma and neutral
atmosphere perturbations. J. Atmos. Solar-Terr. Phys . 64 , 1545-1556.
Tsunoda, R. T. (1998). On polarized frontal structures, type-1 and quasi-periodic echoes
in midlatitude sporadic E. Geophys. Res. Lett . 25 , 2641.
Tsunoda, R. T., Yamamoto, M., Igarashi, K., Hocke, K., and Fukao, S. (1998). Quasi-
periodic radar echoes from midlatitude sporadic E and role of the 5-day planetary
wave. Geophys. Res. Lett. 7 , 951.
Tsunoda, R. T., Buonocore, J. J., Saito, A., Kishimoto, T., Fukao, S., and Yamamoto, M.
(1999). First observations of quasi-periodic radar echoes from Stanford, California.
Geophys. Res. Lett . 26 (7), 995.
Urbina, J., Kudeki, E., Franke, S. J., González, S., Zhou, Q., and Collins, S. C. (2000).
50 MHz radar observations of midlatitude E region irregularities at Camp Santiago,
Puerto Rico. Geophys. Res. Lett . 27 , 2, 853-2, 856.
Vadas, S. L., and Fritts, D. C. (2005). Thermospheric responses to gravity waves: Influ-
ences of increasing viscosity and thermal diffusivity. J. Geophys. Res. 110, D15103,
doi: 10.1029/2004JD005574.