<?xml version="1.0" encoding="utf-8" standalone="yes"?><rss version="2.0" xmlns:atom="http://www.w3.org/2005/Atom"><channel><title>Dynamical Flattening | NJU Astrometry Group</title><link>https://njuastrometry.github.io/en/tag/dynamical-flattening/</link><atom:link href="https://njuastrometry.github.io/en/tag/dynamical-flattening/index.xml" rel="self" type="application/rss+xml"/><description>Dynamical Flattening</description><generator>Hugo Blox Builder (https://hugoblox.com)</generator><language>en-US</language><lastBuildDate>Thu, 21 May 2026 00:00:00 +0000</lastBuildDate><image><url>https://njuastrometry.github.io/media/icon_hu1909758375025618910.png</url><title>Dynamical Flattening</title><link>https://njuastrometry.github.io/en/tag/dynamical-flattening/</link></image><item><title>Astronomical determination of the Earth's dynamical flattening using VLBI observations and IAU 2006/2000 Precession-Nutation Model</title><link>https://njuastrometry.github.io/en/publication/2026-mnras-549-stag953/</link><pubDate>Thu, 21 May 2026 00:00:00 +0000</pubDate><guid>https://njuastrometry.github.io/en/publication/2026-mnras-549-stag953/</guid><description>&lt;p>&lt;strong>Background and method&lt;/strong>&lt;/p>
&lt;p>The Earth&amp;rsquo;s dynamical flattening, $H_{\mathrm d}$, describes the distribution of its principal moments of inertia and is a fundamental parameter in precession-nutation theory:&lt;/p>
&lt;p>$$
H_{\mathrm d}=1-\frac{A+B}{2C},
$$&lt;/p>
&lt;p>where $A$ and $B$ are the equatorial principal moments of inertia and $C$ is the axial moment.&lt;/p>
&lt;p>We estimate this parameter directly from celestial intermediate pole (CIP) coordinates obtained by combining the IAU 2006/2000 precession-nutation model with VLBI celestial pole offsets. The analysis considers four individual analysis-centre series and the IERS C04 combined series, with free core nutation removed before fitting.&lt;/p>
&lt;p>The method explicitly accounts for the dependence of several precession-rate contributions and the main nutation term on $H_{\mathrm d}$, while incorporating additional theoretical corrections. This provides a consistent determination of dynamical flattening within the precession-nutation framework.&lt;/p>
&lt;p>&lt;strong>Main results&lt;/strong>&lt;/p>
&lt;ul>
&lt;li>The estimated dynamical flattening is $H_{\mathrm d}=0.00327380936\pm5\times10^{-11}$, with the quoted uncertainty being formal. This differs from the IAU 2006 adopted value by approximately &lt;strong>4.54 ppm&lt;/strong>.&lt;/li>
&lt;li>The simultaneously estimated frame-bias components are $\delta X=-16603\pm8,\mu\mathrm{as}$ and $\delta Y=-7033\pm8,\mu\mathrm{as}$, in good agreement with the IAU model.&lt;/li>
&lt;li>A separate analysis using &lt;strong>15-year sliding windows with a 2-year step&lt;/strong> estimates long-term changes in $H_{\mathrm d}$ and converts them to changes in the Earth&amp;rsquo;s second zonal gravity coefficient, $J_2$, under the adopted relationship.&lt;/li>
&lt;li>The VLBI-derived $J_2$ variations show a broadly &lt;strong>parabolic long-term trend&lt;/strong>, generally consistent with smoothed satellite laser ranging results, although differences remain for some windows.&lt;/li>
&lt;/ul>
&lt;p>These results demonstrate the value of VLBI precession-nutation observations as an independent probe of long-term changes in the Earth&amp;rsquo;s dynamical figure and provide observational constraints for further refinement of Earth-rotation models.&lt;/p></description></item></channel></rss>