Articles | Volume 17, issue 5
https://doi.org/10.5194/se-17-789-2026
© Author(s) 2026. This work is distributed under the Creative Commons Attribution 4.0 License.
Basic Earth Parameters from VLBI observations using Bayesian inversions in the time domain: updated insights of the Earth's interior
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- Final revised paper (published on 22 May 2026)
- Preprint (discussion started on 30 Sep 2025)
Interactive discussion
Status: closed
Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor
| : Report abuse
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RC1: 'Comment on egusphere-2025-4428', Anonymous Referee #1, 13 Nov 2025
- AC1: 'Reply on RC1', Yuting Cheng, 06 Mar 2026
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RC2: 'Comment on egusphere-2025-4428', Thomas Herring, 02 Feb 2026
- AC2: 'Reply on RC2', Yuting Cheng, 06 Mar 2026
Peer review completion
AR – Author's response | RR – Referee report | ED – Editor decision | EF – Editorial file upload
AR by Yuting Cheng on behalf of the Authors (03 Apr 2026)
Author's response
Author's tracked changes
Manuscript
ED: Publish subject to technical corrections (14 Apr 2026) by Juliane Dannberg
ED: Publish subject to technical corrections (15 Apr 2026) by Susanne Buiter (Executive editor)
AR by Yuting Cheng on behalf of the Authors (21 Apr 2026)
Manuscript
The authors use a Bayesian inversion to recover estimates of Earth parameters from VLBI observations of the Earth’s nutation. The main innovations include the use of a better sampler for the Bayesian inversion, a better ocean tide model and a more flexible recovery of motion to the free core nutation. Comparisons of the revised Earth parameters with previous estimates offer new insights into the structure and dynamics of the Earth’s interior. The results are very interesting, although the manuscript is aimed at an expert audience. I had trouble following parts of the manuscript. These parts could benefit from clarification or more precise descriptions. Most of my comment deal with points of clarification.
Specific Comments
1. The introduction has no references before line 47. Statements are often made without documentation or support. For example, “… the precision (of VLBI) had a major improvement in the late 1980s”. What is “a conventional model” in the definition of the Celestial Pole Offsets?
2. line 59: lager -> larger
3. line 60: “We now have almost 25 years of data with better quality…”. The abstract suggests that 45 years of data are used in the inversion. It appears that “25 years” refers to the additional data available since the MHB 2000 model. This point is clarified in the next paragraph. It might be helpful to move this clarification earlier in the manuscript.
4. The sampling algorithm is updated from a single Metropolis-Hastings sampler to an ensemble Markov Chain Monte Carlo method. Are there references for the original and updated methods? Who is the author of the software package “emcee”?
5. line 100: repeated or nested use of “thanks” makes for an odd sentence.
6. line 118: “the MCMC has more sampling capabilities than the Metropolis-Hastings method”. MCMC is often viewed as a general class of methods, whereas the Metropolis-Hastings is a specific algorithm within that class. A comparison between MCMC and the Metropolis-Hastings methods is confusing.
7. Point of clarification on line 146 - “This suggests that the 0.7 scaling factor applied in the MHB model to reduce ocean tidal effects may have been unnecessary”. Is the idea that updated ocean tidal models have smaller amplitudes, so there is no need to apply a scaling factor to the new models? Presumably some reduction of the ocean tidal model used in MHB 2000 was “necessary”? Could the authors clarify?
8. Table 3: “matter” and “motion” terms refer to changes in moment of inertia and local momentum due to the ocean?
9. Several solutions are used as “observations” in the Bayesian inversion (see Table 3). Readers are given the names of the solutions and the processing software, but few other details are stated. For example, usn2024b.eoxy and gsf2023a.eoxy use the same processing software. What is the difference between these solutions? The authors note that these different solutions give similar results in the inversion. How should readers assess this statement without information about the input solutions?
10. line 186: Does the calculation of “beta” from PREM include the anelastic contribution?
11. line 191: What value of electrical conductivity is assumed in the calculation of the rms radial field (=0.75 mT)? How is a “realistic” conductivity assessed? How is a “realistic” rms radial field assessed?
12. line 276: “The halved Re(K^ICB) values,…..” . The earlier text makes it clear that the “halved values” refer to the MHB 2000 model. Why not be specific in the “Concluding remarks”?