available measured data is to form neural network model for
TEC values. It is proven that this model is easy to be realized
and it can determine TEC values quickly based on space and
time information of the signal propagation in the ionosphere.
Previously shown results for used FPR_RBF neural model for
FR angle estimation for winter and summer period in the
Mediterrean region provide good evidence that the use of NNs
to solve this problem is a good choice. The results also prove
that neural network models are a good alternative for the
expensive and hardware demanding numerical models but also
for software for description of the ionosphere influence on EM
propagating waves. This models are also good alternative for
slow and rough estimation of manual reading of TEC values.
Fig. 9. Ionospheric FR angle of the P-SAR signal (f = 440 MHz) and L-SAR
signal (f = 1250 MHz) obtained by FPR-RBF model
Fig. 10. Ionospheric FR angle of the P-SAR signal (f = 440 MHz) and L-SAR
signal (f = 1250 MHz) obtained by FPR-RBF model
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