In situ collection of dust grains falling from Saturn’s rings into its atmosphere

Author:

Hsu Hsiang-Wen1ORCID,Schmidt Jürgen2ORCID,Kempf Sascha1ORCID,Postberg Frank34,Moragas-Klostermeyer Georg5ORCID,Seiß Martin6,Hoffmann Holger6ORCID,Burton Marcia7,Ye ShengYi8ORCID,Kurth William S.8ORCID,Horányi Mihály1,Khawaja Nozair34,Spahn Frank6,Schirdewahn Daniel6,O’Donoghue James9ORCID,Moore Luke10ORCID,Cuzzi Jeff11,Jones Geraint H.1213ORCID,Srama Ralf514ORCID

Affiliation:

1. Laboratory for Atmospheric and Space Physics, University of Colorado–Boulder, Boulder, CO, USA.

2. Astronomy Research Unit, University of Oulu, Oulu, Finland.

3. Institut für Geowissenschaften, Universität Heidelberg, Heidelberg, Germany.

4. Institut für Geologische Wissenschaften, Freie Universität Berlin, Berlin, Germany.

5. Institut für Raumfahrtsysteme, Universität Stuttgart, Stuttgart, Germany.

6. Institut für Physik und Astronomie, Universität Potsdam, Potsdam, Germany.

7. Jet Propulsion Laboratory, Pasadena, CA, USA.

8. Department of Physics and Astronomy, University of Iowa, Iowa City, IA, USA.

9. NASA Goddard Space Flight Center, Greenbelt, MD, USA.

10. Center for Space Physics, Boston University, Boston, MA, USA.

11. NASA Ames Research Center, Moffett Field, CA, USA.

12. Mullard Space Science Laboratory, University College London, Holmbury St. Mary, Dorking, UK.

13. The Centre for Planetary Sciences at University College London/Birkbeck, London, UK.

14. Center for Astrophysics, Space Physics, and Engineering Research, Baylor University, Waco, TX, USA.

Abstract

Cassini's final phase of exploration The Cassini spacecraft spent 13 years orbiting Saturn; as it ran low on fuel, the trajectory was changed to sample regions it had not yet visited. A series of orbits close to the rings was followed by a Grand Finale orbit, which took the spacecraft through the gap between Saturn and its rings before the spacecraft was destroyed when it entered the planet's upper atmosphere. Six papers in this issue report results from these final phases of the Cassini mission. Dougherty et al. measured the magnetic field close to Saturn, which implies a complex multilayer dynamo process inside the planet. Roussos et al. detected an additional radiation belt trapped within the rings, sustained by the radioactive decay of free neutrons. Lamy et al. present plasma measurements taken as Cassini flew through regions emitting kilometric radiation, connected to the planet's aurorae. Hsu et al. determined the composition of large, solid dust particles falling from the rings into the planet, whereas Mitchell et al. investigated the smaller dust nanograins and show how they interact with the planet's upper atmosphere. Finally, Waite et al. identified molecules in the infalling material and directly measured the composition of Saturn's atmosphere. Science , this issue p. eaat5434 , p. eaat1962 , p. eaat2027 , p. eaat3185 , p. eaat2236 , p. eaat2382

Funder

National Aeronautics and Space Administration

H2020 European Research Council

Deutsche Forschungsgemeinschaft

DLR German Aerospace Center

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

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