Figure 1.
(a) Locations of the earthquake and GNSS stations. (b) and (c) are observations and synthetics in PPP and RP. S1-S2 represents the RP waveform with S2 as the reference station. While precise PPP requires a delay of as much as 1–2 weeks, RP offers rapid, near real-time waveform (S1–S2) with comparable accuracy. PPP waveforms can be directly matched with synthetics, whereas RP waveform should be matched with differential synthetics.

(a) Locations of the earthquake and GNSS stations. (b) and (c) are observations and synthetics in PPP and RP. S1-S2 represents the RP waveform with S2 as the reference station. While precise PPP requires a delay of as much as 1–2 weeks, RP offers rapid, near real-time waveform (S1–S2) with comparable accuracy. PPP waveforms can be directly matched with synthetics, whereas RP waveform should be matched with differential synthetics.

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