Mv. Goldman et al., THEORY OF CONVECTIVE SATURATION OF LANGMUIR-WAVES DURING IONOSPHERIC MODIFICATION OF A BARIUM CLOUD, Journal of atmospheric and solar-terrestrial physics, 59(18), 1997, pp. 2335-2350
In recent experiments (Djuth, F. T., Sulzer, M. P., Elder, J. H. and G
roves, K. M. (1995) Journal of Geophysical Research, 100, 17,347), a p
arametric decay instability was excited by an ordinary-wave HF pump du
ring an ionospheric chemical release from a rocket over Arecibo, PR, w
hich created an artificial 'barium ionosphere,' with peak plasma frequ
ency above the pump frequency, and a density gradient with a (short) 5
km scale length. Simultaneous incoherent scattering measurements reve
aled a strong initial asymmetry in the amplitudes of almost vertically
upgoing versus downgoing measured plasma waves. We can account for th
is asymmetry in terms of linear convective saturation of parametricall
y unstable plasma waves propagating over a range of altitudes along ge
ometric optics ray paths. Qualitative features of the frequency spectr
um of the measured downgoing wave are in agreement with this model, al
though the theoretically predicted spectrum is narrower than observed.
The observed altitude localization of the enhanced spectrum to a few
range cells is consistent with the theory. (C) 1997 Elsevier Science L
td.