All Tables

Table 1: The range of frequency bands for estimation of a non-tidal signal. The last column refers to components of $\vec{q}_e(t)$ vector of perturbational rotation that were estimated.
Table 2: The weighted root mean squares of the differences between estimates of the Earth rotation model from analysis of VLBI observations and the USNO Finals EOP model for the period of [1996.0, 2006.0]. The statistics in rows 1 and 2 correspond to solution B, which follows the proposed approach. The statistics in row 3 correspond to solution gsf2006c, which follows the traditional approach.
Table 3: Numerical values of the a priori Earth rotation model parameters used in data reduction.