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Application of the locality principle to radio occultation studies of the Earth's atmosphere and ionosphere

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Academic year: 2017

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Figure 1. Scheme of radio occultation measurements.
Figure 2. Comparison of the refractive attenuations X a (h) and X p (h) and their polynomial approximations, corresponding to the FORMOSAT-3 RO measurements carried out on 18 October and 11 April 2008 (left and right plots, respectively)
Figure 4. Left plot – Comparison of the polynomial approximations of refractive attenuations X a (h), X p (h) (curves 1–4, indexes “p” and
Figure 5. (a) Comparison of the refractive attenuations X a (h), X p (h) found from the RO intensity and eikonal data at GPS frequency F1 (curves 1 and 2, respectively)
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