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Cassini's Grand Finale Unveils Variations in Saturn's D Ring influx
Joshua has analysed plasma measurements from multiple instruments on the Cassini spacecraft gathered during the last few orbits of the mission, the "Grand Finale", which sampled the region between the rings and the atmosphere before Cassini's eventual disintegration in Saturn's atmosphere in September 2017.
Cassini's Grand Finale Unveils Variations in Saturn's D Ring influx
by Staff Writers
Uppsala, Sweden (SPX) Nov 28, 2023

In a significant addition to our understanding of Saturn's atmospheric dynamics, Joshua Dreyer is poised to present his doctoral thesis at the Swedish Institute of Space Physics (IRF) and Uppsala University. His research, which scrutinizes the effects of material from Saturn's innermost D ring falling into its upper atmosphere, marks a novel chapter in space exploration and planetary science.

The thesis, titled "Diving Deep into Saturn's Equatorial Ionosphere with Cassini: Insights from the Grand Finale," delves into the composition of plasma - charged particles - in the upper segment of Saturn's atmosphere. It builds upon the foundational knowledge derived since the discovery of the ring influx, offering a current perspective on this celestial phenomenon.

Dreyer's research, conducted through meticulous analysis of plasma measurements from the Cassini spacecraft, has revealed that the signatures of the ring influx are notably variable. "My research shows the signatures of the ring influx to be surprisingly variable throughout any one orbit and between orbits, which may indicate that the ring influx itself varies a lot," explains Joshua. This variability suggests a more complex interaction between the D ring and Saturn's atmosphere than previously understood.

The Cassini mission, a cornerstone in planetary exploration, concluded its journey with the "Grand Finale" orbits, which involved close passes between Saturn's rings and atmosphere before the spacecraft's deliberate descent into the planet's atmosphere in September 2017. During these final orbits, Cassini gathered crucial data about the interaction between the ring material and Saturn's atmosphere.

Dreyer's findings indicate that the infalling ring material, primarily composed of water ice and other heavy species, significantly shapes Saturn's equatorial ionosphere. This influx introduces volatile species into the atmosphere, resulting in a more intricate plasma composition. This insight is particularly relevant given that the main constituents of Saturn's upper atmosphere are hydrogen and helium.

An unexpected twist in Dreyer's research was the discovery of a timestamp shift in the ion data, unveiled during the investigation of ring shadowing signatures in the ionospheric data. This correction aligned the electron and ion data, even on small scales, providing a more accurate understanding of the ring material's impact.

Dreyer, who commenced his academic journey in Germany and continued his master's studies in Uppsala in 2017, will defend his thesis at 13:00 on Thursday, 23 November, in Uppsala, Sweden. The faculty examiner for his thesis defense is Prof. Ingo Muller-Wodarg from Imperial College London.

This research not only enhances our knowledge of Saturn's atmospheric dynamics but also contributes to the broader understanding of planetary atmospheres and ring systems. As we continue to explore our solar system, studies like Dreyer's provide vital insights into the complex interplay between planetary bodies and their surrounding environments.

Research Report:Diving Deep into Saturn's Equatorial Ionosphere with Cassini: Insights from the Grand Finale

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