Linking Zonal Winds and Gravity: The Relative Importance of Dynamic Self Gravity
Johannes Wicht, Wieland Dietrich, Paula Wulff, Ulrich R., Christensen

TL;DR
This paper investigates the significance of Dynamic Self Gravity (DSG) in planetary gravity measurements, showing it is a first-order effect for low degrees and should be included in models to improve accuracy.
Contribution
The study provides an analytical approach to quantify DSG's impact on gravity harmonics, demonstrating its importance for degrees l=2 to about l=10 in planetary interior modeling.
Findings
DSG significantly affects low-degree gravity harmonics (l=2 to 4).
Impact of DSG decreases with increasing harmonic degree.
Including DSG improves the accuracy of gravity-based zonal flow inferences.
Abstract
Recent precise measurements at Jupiter's and Saturn's gravity fields constrain the properties of the zonal flows in the outer envelopes of these planets. A simplified dynamic equation, sometimes called the thermal wind or thermo-gravitational wind equation, establishes a link between zonal flows and the related buoyancy perturbation, which in turn can be exploited to yield the dynamic gravity perturbation. Whether or not the action of the dynamic gravity perturbation needs to be explicitly included in this equation, an effect we call the Dynamic Self Gravity (DSG), has been a matter of intense debate. We show that, under reasonable assumptions, the equation can be solved (semi) analytically. This allows us to quantify the impact of the DSG on each gravity harmonic, practically independent of the zonal flow or the details of the planetary interior model. The impact decreases with growing…
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