Ocean loading tides introduce earth surface displacements at the centimetre level. We show that these effects can be recovered from GP5 data using long time-series from Precise Point Positioning solutions. The formal uncertainty of the observed ocean loading parameters can be as low as half a millimetre. Observations from 11 stations are used.
CITATION STYLE
Scherneck, H. G., Johansson, J. M., & Webb, F. H. (2000). Ocean loading tides in GPS and rapid variations of the frame origin (pp. 32–40). https://doi.org/10.1007/978-3-642-59742-8_6
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