Physics
Scientific paper
May 2006
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2006agusmsa44a..04c&link_type=abstract
American Geophysical Union, Fall Meeting 2007, abstract #SA44A-04
Physics
2411 Electric Fields (2712), 2443 Midlatitude Ionosphere, 2471 Plasma Waves And Instabilities (2772)
Scientific paper
Using the Arecibo incoherent scatter radar, Behnke [1979] observed line of sight Doppler velocities in the F region exceeding 400 m/s, together with sharp 80 km rises in the F layer altitude. Although this observation was for some time attributed to the Perkins instability, the growth rate of the Perkins instability is discouragingly small. Tsunoda and Cosgrove [2001] suggested that a more likely source was a coupled effect involving a sporadic E (Es) layer and the F layer. They noted the apparent presence of positive feedback between a Hall-current-driven polarization process in Es layers, and a Pedersen-current-driven process in the F region. Cosgrove and Tsunoda [2002b, 2003] have since shown that Es layers are unstable with properties similar to those of the Perkins instability, motivating the idea that the two instabilities may couple. Cosgrove and Tsunoda [2004a, b] derived the linear growth rate for the coupled system of an Es layer and the F layer, thus realizing a unified formalism for the Perkins and Es layer instabilities. In the present paper we present a numerical simulation of the two-dimensional nonlinear evolution of the unstable coupled system. The results show that the time scale for the development of structure in the F region is significantly reduced when a Es layer is present. The Es layer evolution is highly nonlinear compared to the F layer evolution, and exhibits a wave breaking phenomenon that is associated with a strong electric field pulse. The result of the electric field pulse is a sharp modulation of the F layer altitude.
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