Research Article
The Use of the Total Electron Content Measured by Navigation Satellites to Estimate Ionospheric Conditions
Table 1
Deviations of frequencies calculated according to the hyperbolic approximation from experimental values in April 2014.
| 1 | 2 | 3 | 4 | 5 | 6 | 7 | 8 | 9 | 10 | station | , | ā | IRI | Rec | Stat | Reg 2 | Reg 4 | Lat 1 | Lat 2 |
| Juliusruh | 3295.5 | f | 0.73 | 0.41 | 0.43 | 0.68 | 0.67 | 1.03 | 0.57 | Reg 2 | 273.2 | d | 1.44 | 0.52 | 0.49 | 0.67 | 0.68 | 1.07 | 0.64 | Athens | 5929.3 | f | 0.91 | 0.36 | 0.46 | 0.56 | 0.48 | 0.52 | 0.58 | Reg 2 | 253.2 | d | 1.31 | 0.44 | 0.74 | 0.52 | 0.59 | 0.87 | 0.51 | Grahams | 3788.7 | f | 0.8 | 0.4 | 0.54 | 0.77 | 0.59 | 0.73 | 0.73 | Lat 2 | 293.2 | d | 1.54 | 0.46 | 0.62 | 0.84 | 0.75 | 0.82 | 0.77 | Longyear | 4947.1 | f | 0.7 | 0.43 | 0.62 | 0.6 | 0.58 | 0.82 | 0.58 | Lat 2 | 244.2 | d | 0.69 | 0.49 | 0.73 | 0.69 | 0.69 | 1.01 | 0.63 | Thule | 692.7 | f | 0.51 | 0.14 | 0.15 | 0.56 | 0.42 | 0.47 | 0.59 | 437.6 | d | 0.55 | 0.1 | 0.13 | 0.51 | 0.46 | 0.64 | 0.54 | Millstone | 4864.4 | f | 0.9 | 0.5 | 0.47 | 0.48 | 0.46 | 0.67 | 0.49 | Lat 1 | 265.4 | d | 1.38 | 0.67 | 0.67 | 0.65 | 0.81 | 0.81 | 0.8 | Beijing | 5402.8 | f | 1.17 | 0.49 | 0.61 | 0.61 | 0.58 | 0.7 | 0.62 | Reg 4 | 263.9 | d | 1.99 | 0.42 | 0.64 | 0.45 | 0.51 | 0.84 | 0.45 | Kokubunji | 6176.7 | f | 1.29 | 0.47 | 0.65 | 0.61 | 0.69 | 0.85 | 0.62 | Reg 4 | 228.4 | d | 2.11 | 0.55 | 0.66 | 0.56 | 0.7 | 0.96 | 0.56 | Niue | 4874.7 | f | 1.85 | 1.15 | 1.36 | 1.35 | 1.28 | 1.43 | 1.29 | Reg 4 | 285 | d | 1.67 | 0.71 | 1 | 0.73 | 0.85 | 1.11 | 0.67 | Cocos | 5467.3 | f | 1.43 | 0.55 | 0.68 | 0.86 | 0.62 | 0.65 | 0.82 | Lat 2 | 267.8 | d | 1.66 | 0.52 | 0.77 | 0.88 | 0.67 | 0.8 | 0.83 | Mawson | 1466.2 | f | 0.91 | 0.27 | 0.37 | 1 | 0.85 | 1.02 | 0.92 | Lat 2 | 386.8 | d | 1.12 | 0.12 | 0.21 | 0.8 | 0.98 | 0.98 | 0.81 |
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