Saturn’s magnetic field revealed by the Cassini Grand Finale

Author:

Dougherty Michele K.1ORCID,Cao Hao23ORCID,Khurana Krishan K.4ORCID,Hunt Gregory J.1ORCID,Provan Gabrielle5ORCID,Kellock Stephen1ORCID,Burton Marcia E.6,Burk Thomas A.6,Bunce Emma J.5ORCID,Cowley Stanley W. H.5ORCID,Kivelson Margaret G.47ORCID,Russell Christopher T.4ORCID,Southwood David J.1ORCID

Affiliation:

1. Physics Department, The Blackett Laboratory, Imperial College London, London, SW7 2AZ, UK.

2. Department of Earth and Planetary Sciences, Harvard University, 20 Oxford Street, Cambridge, MA 02138, USA.

3. Division of Geological and Planetary Sciences, California Institute of Technology, 1200 E California Boulevard, Pasadena, CA 91125, USA.

4. Department of Earth, Planetary, and Space Sciences, University of California, Los Angeles, Los Angeles, CA 90025, USA.

5. Department of Physics and Astronomy, University of Leicester, Leicester LE1 7RH, UK.

6. Jet Propulsion Laboratory, California Institute of Technology, 4800 Oak Grove Drive, Pasadena, CA 91109, USA.

7. Department of Climate and Space Sciences and Engineering, University of Michigan, Ann Arbor, MI 40109, 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

Jet Propulsion Laboratory

UK STFC

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

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