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Remote sensing of tropospheric turbulence using GPS radio occultation

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Figure

Figure 1. Global map of altitudinal average (1–4 km altitudes) scintillation index derived from the COSMIC RO data for January, April, July,and October 2008.
Figure 3. Histogram of σ 2I COSMIC RO averaged over 1–8 km: (a) tropics, (b) midlatitude, and (c) high latitude.
Figure 4. The index of refraction structure parameter C2n inferred from CT signal amplitude of COSMIC RO data.
Figure 5. (a, b) Example refractivity profile employed as an input for the multi phase screen (MPS) simulation runs;and Arctic, north of Alaska); and (c) scintillation indexσ 2I profiles inferred from MPS model runs; (d) σ 2I inferred from COSMIC RO observations (averages over Central Pacific, New Mexico, (e) C2n derived from σ 2I MPS model.

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