EPSC Abstracts
Vol. 19, EPSC2026-614, 2026, updated on 02 Jul 2026
https://doi.org/10.5194/epsc2026-614
Europlanet Science Congress 2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
Poster | Tuesday, 08 Sep, 18:00–19:30 (CEST), Display time Tuesday, 08 Sep, 08:30–19:30| Foyer 3, F3.12
Shallow Water Simulations of the Latitudinal Drift of Saturn’s Anticyclonic Vortex (AV)
Aida Flix-Bellmunt1, Agustín Sánchez-Lavega2, Enrique García-Melendo1, Arnau Miró1, and Manel Soria1
Aida Flix-Bellmunt et al.
  • 1Universitat Politècnica de Catalunya (UPC), Terrassa, Spain
  • 2Universidad del País Vasco (UPV/EHU), Bilbao, Spain

The AV is an anticyclonic vortex on Saturn that formed at approximately 40°N following the Great White Spot (GWS) of 2010 and has remained active since then. During its first year, the vortex migrated northward to 44°N and then returned to 43°N, where it has since exhibited latitudinal oscillations (Hueso et al., 2020). This migration is theoretically attributed to the β-drift effect, which is driven by vorticity gradients and controlled by the barotropic beta parameter (βb), i.e., the sum of the relative and planetary vorticity gradients. For anticyclones, a poleward migration occurs when βb < 0, while the vortex moves equatorward when βb > 0. Analyzing the zonal wind profiles retrieved with Cassini during 2004—2009 (García-Melendo et al., 2011), Trammell et al. (2016) calculated the relative vorticity and presented a latitudinal profile. From it, they found that the AV formed at a region where βb < 0 and identified 43°N as an equilibrium point (βb = 0). In this study, we employed a Shallow Water model to simulate the positional evolution of the AV after its formation for 100—150 days, limited by numerical dissipation. We retrieved the northward drift rate and compared it to the observed 2011 migration rate (Hueso et al., 2020). The simulations provide further insight into the influence of the zonal wind profile shape on vortex drifting. Furthermore, the retrieved migration velocity serves as a validation benchmark for the numerical model.

References

García-Melendo, E., Pérez-Hoyos, S., Sánchez-Lavega, A., & Hueso, R. (2011). Saturn’s zonal wind profile in 2004–2009 from Cassini ISS images and its long-term variability. Icarus, 215(1), 62–74. https://doi.org/10.1016/j.icarus.2011.07.005

Hueso, R., Sánchez-Lavega, A., Rojas, J. F., Simon, A. A., Barry, T., del Río-Gaztelurrutia, T., Antuñano, A., Sayanagi, K. M., Delcroix, M., Fletcher, L. N., García-Melendo, E., Pérez-Hoyos, S., Blalock, J., Colas, F., Gómez-Forrellad, J. M., Gunnarson, J. L., Peach, D., & Wong, M. H. (2020). Saturn atmospheric dynamics one year after Cassini: Long-lived features and time variations in the drift of the Hexagon. Icarus, 336, 113429. https://doi.org/10.1016/j.icarus.2019.113429

Trammell, H. J., Li, L., Jiang, X., Pan, Y., Smith, M. A., Bering III, E. A., Hörst, S. M., Vasavada, A. R., Ingersoll, A. P., Janssen, M. A., West, R. A., Porco, C. C., Li, C., Simon, A. A., & Baines, K. H. (2016). Vortices in Saturn's Northern Hemisphere (2008–2015) observed by Cassini ISS. Journal of Geophysical Research: Planets, 121(9), 1814–1826. https://doi.org/10.1002/2016JE005122

How to cite: Flix-Bellmunt, A., Sánchez-Lavega, A., García-Melendo, E., Miró, A., and Soria, M.: Shallow Water Simulations of the Latitudinal Drift of Saturn’s Anticyclonic Vortex (AV), Europlanet Science Congress 2026, The Hague, The Netherlands, 7–11 Sep 2026, EPSC2026-614, https://doi.org/10.5194/epsc2026-614, 2026.