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Diurnal variations in integrated water vapor derived from a GPS ground network in the Volga–Ural region of Russia

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Figure

Table 2. GPS–radiosonde comparison.
Figure 1.
Figure 1. Mean diurnal variations in surface water vapor densitycurve) data at four GPS stations for winter ρ0 (dotted curve), IWV from GPS (solid curve) and ERA-Interim (dashed (a), spring (b), summer (c) and autumn (d).
Figure 2. Amplitude (a) and time at the maximum (b) of diurnal harmonic.
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