# Hydrodynamic simulations of moonlet induced propellers in Saturn's   rings: Application to Bleriot

**Authors:** Martin Sei{\ss}, Nicole Albers, Miodrag Sremcevic, J\"urgen Schmidt,, Heikki Salo, Michael Seiler, Holger Hoffmann, Frank Spahn

arXiv: 1701.04641 · 2018-10-25

## TL;DR

This paper presents hydrodynamic simulations of moonlet-induced propellers in Saturn's rings, validating the model against N-body simulations and Cassini observations, and applies it to the large propeller Bleriot to estimate moonlet properties.

## Contribution

The study develops an advanced hydrodynamic model for propellers, confirming scaling laws and analytical solutions, and successfully simulates large propellers like Bleriot beyond N-body capabilities.

## Key findings

- Hydrodynamic simulations agree with N-body results.
- Model fits Cassini UVIS data for Bleriot, estimating moonlet size.
- Derived ring viscosity and velocity parameters consistent with observations.

## Abstract

One of the biggest successes of the Cassini mission is the detection of small moons (moonlets) embedded in Saturn's rings which cause S-shaped density structures in their close vicinity, called propellers (Spahn and Sremcevic 2000; Tiscareno et al. 2006; Sremcevic et al. 2007). Here, we present isothermal hydrodynamic simulations of moonlet-induced propellers in Saturn's A ring which denote a further development of the original model (Spahn and Sremcevic 2000). We find excellent agreement between these new hydrodynamic and corresponding N-body simulations. Furthermore, the hydrodynamic simulations confirm the predicted scaling laws (Spahn and Sremcevic 2000) and the analytical solution for the density in the propeller gaps (Sremcevic et al. 2002). Finally, this mean field approach allows us to simulate the pattern of the giant propeller Bleriot, which is too large to be modeled by direct N-body simulations. Our results are compared to two stellar occultation observations by the Cassini Ultraviolet Imaging Spectrometer (UVIS), that intersect the propeller Bleriot. Best fits to the UVIS optical depth profiles are achieved for a Hill radius of 590 m, which implies a moonlet diameter of about 860 m. Furthermore, the model favours a kinematic shear viscosity of the surrounding ring material of $\nu_0 = 340$ cm^2/s, a dispersion velocity in the range of 0.3 cm/s $< c_0 <$ 1.5 cm/s, and a fairly high bulk viscosity $7 < \xi_0/\nu_0 < 17$. These large transport values might be overestimated by our isothermal ring model and should be reviewed by an extended model including thermal fluctuations.

## Full text

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## Figures

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## References

62 references — full list in the complete paper: https://tomesphere.com/paper/1701.04641/full.md

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Source: https://tomesphere.com/paper/1701.04641