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Long-Term Evaluation of Ocean Tidal Variation Models of Polar Motion and UT1

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/persons/resource/karbon

Karbon,  Maria
External Organizations;

/persons/resource/balidak

Balidakis,  K.
External Organizations;

/persons/resource/sanbelpa

Belda,  Santiago
External Organizations;

/persons/resource/nilsson

Nilsson,  T.
1.1 Space Geodetic Techniques, 1.0 Geodesy, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum;

/persons/resource/janh

Hagedoorn,  Jan
External Organizations;

/persons/resource/schuh

Schuh,  H.
1.1 Space Geodetic Techniques, 1.0 Geodesy, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum;

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Citation

Karbon, M., Balidakis, K., Belda, S., Nilsson, T., Hagedoorn, J., Schuh, H. (2018): Long-Term Evaluation of Ocean Tidal Variation Models of Polar Motion and UT1. - Pure and Applied Geophysics, 175, 5, 1611-1629.
https://doi.org/10.1007/s00024-018-1866-1


Cite as: https://gfzpublic.gfz-potsdam.de/pubman/item/item_3471892
Abstract
Recent improvements in the development of VLBI (very long baseline interferometry) and other space geodetic techniques such as the global navigation satellite systems (GNSS) require very precise a-priori information of short-period (daily and sub-daily) Earth rotation variations. One significant contribution to Earth rotation is caused by the diurnal and semi-diurnal ocean tides. Within this work, we developed a new model for the short-period ocean tidal variations in Earth rotation, where the ocean tidal angular momentum model and the Earth rotation variation have been setup jointly. Besides the model of the short-period variation of the Earth’s rotation parameters (ERP), based on the empirical ocean tide model EOT11a, we developed also ERP models, that are based on the hydrodynamic ocean tide models FES2012 and HAMTIDE. Furthermore, we have assessed the effect of uncertainties in the elastic Earth model on the resulting ERP models. Our proposed alternative ERP model to the IERS 2010 conventional model considers the elastic model PREM and 260 partial tides. The choice of the ocean tide model and the determination of the tidal velocities have been identified as the main uncertainties. However, in the VLBI analysis all models perform on the same level of accuracy. From these findings, we conclude that the models presented here, which are based on a re-examined theoretical description and long-term satellite altimetry observation only, are an alternative for the IERS conventional model but do not improve the geodetic results.