Abstract
Jupiter’s Great Red Spot (GRS) is among the largest discrete weather features in the Solar System. Although observed for at least 200 years, the GRS is shrinking, particularly in the past 50 years. Studies of long-lived terrestrial anticyclonic features, known as blocks, demonstrate that they can be sustained, in part, by interactions with transient vortices. Motivated by these results and observations of the GRS absorbing smaller vortices, we conduct three-dimensional simulations of a GRS-like vortex. Control simulations omit forced vortex interactions, while a set of experimental simulations include GRS interactions with transient anticyclones of varying frequency and intensity. Comparison of these simulations allows isolation of the role of such mergers in the GRS evolution. We find that the GRS is larger following periodic vortex interactions relative to control simulations without mergers. Similarly, analysis of upper troposphere eddy potential vorticity and dynamic tropopause potential temperature anomalies suggests the GRS is strengthened by vortex interactions. The degree to which the GRS is sustained increases with interaction frequency and transient anticyclone intensity. These results are consistent with terrestrial blocking dynamics and support the theory that the GRS is modulated by persistent interactions with smaller vortices.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.