The process of formation and further evolution of strong electron concentra
tion inhomogeneities in the F-layer of the ionosphere created by the field
of a powerful radio wave is investigated. Numerical simulations are employe
d to obtain the associated ray propagation trajectories which determine com
munication properties under such circumstances. The simulations involve the
formulas obtained for the problem of one-dimensional non-stationary thermo
-diffusion and diffusion spreading of the electron component for ionospheri
c plasmas. The numerical model takes into account the real boundary conditi
ons in the E- and F-layers of the middle-latitude ionosphere and the altitu
dinal distribution of electron transport coefficients, as well as the ioniz
ation-recombination balance in the ionosphere. The ray tracing model is int
roduced to examine changes of the probing waves trajectories due to reflect
ions from heating induced ionospheric plasma inhomogeneities at various ran
ges. Using the extended Hamiltonian formulation for the ray equations, the
changes of ray trajectories passing through the heating area in the upper i
onosphere are examined for different regimes of ionospheric plasma heating.
The results show that local resonance heating is conducive to broader band
width and that, in the presence of sharp gradients, reflection takes place
at higher frequencies than in the quiescent ambient ionospheric plasma. It
has been found that in certain cases reflection occurs well into the 1 GHz
band. This result is important for both communications between ground based
stations and for wave propagation involving low altitude missiles and sate
llites or re-entering space vehicles. It was found that, for adaptive heati
ng which is closely related to natural phenomena in the high latitude ionos
phere, the effect of bandwidth broadening is less meaningful. The ray propa
gation algorithm used takes into account the loss properties of the plasma
medium, although it has been found that for the presently simulated paramet
ers these effects are marginal. (C) 1998 Elsevier Science Ltd. All rights r
eserved.