Summary
From measurements made with an Askania tidal apparatus at a reference station it is possible to derive the correction parameters k and τ, if required, for reducing the gravimetric factors δ and phase lags ξ to a unified system, Eq. (2). It is suggested that several tidal waves be used to determine k and τ and to take the weighted mean as the resultant value. Suitable weights have also been derived, Eq. (7).
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References
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Dedicated to RNDr Jan Pícha, CSc., on his 60th Birthday
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Šimon, Z. Determination of the correction parameters of an askania gravimetric tidal apparatus. Stud Geophys Geod 22, 148–153 (1978). https://doi.org/10.1007/BF01614038
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DOI: https://doi.org/10.1007/BF01614038