Celestial pole offsets in $\mathrm{d}X$ after removing free core nutation.Context. In 2006, the IAU adopted a new precession theory, called the IAU 2006. The time variation of the Earth’s dynamical flattening $J_{2}$ was considered in this model as an important contribution to the precession rate in longitude. However, a linear $J_{2}$ trend, which was valid at that time, is no longer a good approximation and may limit the accuracy of the theory. Aims. We investigated the contribution of latest nonlinear $J_{2}$ variation in developing the precession quantities of the equator. Methods. Using the most recent satellite laser ranging data, we modeled the Earth’s $J_{2}$ long-term variation using a parabola. It was implemented in calculating the polynomial expressions for precession quantities with a method similar to the IAU 2006 approach. Results. The updated precession solution is clearly more consistent with VLBI observations and can reduce most of the curvature signals in the CPO series. The validity of using a parabolic $J_{2}$ variation in precession development is confirmed. Conclusions. The new precession can be regarded as an update of the IAU 2006 model, and thus we named it IAU $2006_{J_{2}}$. Since the improvement shown by the tests with VLBI observations is quite significant, we propose that a serious discussion for updating the IAU precession be carried out by the IAU/IAG Joint Working Group: Consistent Improvement of the Earth’s Rotation Theory (CIERT). It could also be considered for the next update of the IERS Conventions which took effect more than 15 years ago.
The IAU 2006 precession model incorporates a linear trend in Earth’s gravitational coefficient $J_{2}$, which characterizes its oblateness. However, satellite laser ranging observations extending from 1976 to 2025 show that the long-term evolution of $J_{2}$ is better represented by a parabola.
We use these observations to determine an updated empirical model of $J_{2}$ and incorporate it into the integration of the precession equations. The resulting solution, named IAU $2006_{J_{2}}$, follows the framework of the IAU 2006 model while updating the polynomial expressions for the precession quantities.
The results provide observational support for updating the precession model within the IAU 2006 framework. The paper proposes the solution for consideration by the IAU/IAG CIERT working group and in a future revision of the IERS Conventions.
Further work on the corresponding nutation corrections is needed to ensure consistency between precession and nutation when the time variation of Earth’s dynamical flattening is taken into account.