| 英文摘要 |
This study evaluates the feasibility of using Global Navigation Satellite System Interferometric Reflectometry (GNSS-IR) to establish Taiwan’s vertical datum. The co-located GNSS station and tide gauge at Kaohsiung Harbor were used, covering observations from 2005 to 2016. GNSS signal-to-noise ratio (SNR) data were analyzed to retrieve reflector heights, and Precise Point Positioning (PPP) was applied to estimate antenna ellipsoidal heights, enabling the derivation of ellipsoidal sea surface heights. To improve retrieval accuracy, several error sources were considered, including sea surface dynamics, tropospheric refraction, and inter-frequency bias. In addition, tidal harmonic analysis was incorporated to constrain spectral peak identification in the Lomb–Scargle periodogram (LSP). The results show strong agreement between GNSS-IR and tide gauge observations, with a correlation coefficient of 0.87, a regression slope of 0.99, and a coefficient of determination (𝑅2 ) of 0.9999. These findings indicate that GNSS-IR effectively captures sea level variability. However, a systematic datum offset of -12.7 cm was observed between the two datasets. The most likely sources of this discrepancy are systematic vertical-related errors and sea state bias, although their respective contributions require further investigation. Overall, after accounting for datum differences, GNSS-IR demonstrates high consistency and reliability in monitoring sea level variations. The results confirm that GNSS-IR is a promising technique for estimating long-term mean ellipsoidal sea surface height and can serve as a complementary or alternative observation method to tide gauges, especially in regions with sparse observations. |