Peculiar rainbows in Saturn’s E ring: Uncovering luminous bands near Enceladus

We report observations of stripe-like features in Enceladus’ plumes captured simultaneously by Cassini’s VIMS-IR and ISS NAC instruments during flyby E17, with similar patterns seen in VIMS-IR data from flyby E13 and E19. These parallel stripes, inclined at approximately 16°to the ecliptic and 43°to Saturn’s ring plane, appear continuous across images when projected in the J2000 frame. A bright stripe, most visible at wavelengths around 5 μ m , acts as the zeroth-order diffraction peak of a reflection grating with an estimated groove spacing of 0.12–2.60 mm, while adjacent stripes are attributed to higher-order diffraction peaks. We suggest that this light-dispersing phenomenon originates from an inclined periodic structure within Saturn’s E ring. This structure, constrained between Saturn’s G-ring and Rhea’s orbit, likely consists of fresh ice particles supplied by Enceladus’ plumes. • Cassini’s ISS and VIMS uncover luminous, rainbow-like stripes near Enceladus. • Stripes show chromatic shifts, indicating diffraction by a millimetre-sized structure. • A bright band at 5 μ m lies at the centre of the stripe pattern. • Spectra hint at fresh, crystalline ice with large grains and solid CO 2 traces. • Discovery suggests an inclined, periodic ice formation in Saturn’s E ring.

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Publication Details

Journal
Icarus
Published
2025-06-02
DOI
https://doi.org/10.1016/j.icarus.2025.116650
Primary Topic
Astro and Planetary Science
Type
article
Field-Weighted Citation Impact
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article

Peculiar rainbows in Saturn’s E ring: Uncovering luminous bands near Enceladus

Matthew D. Kenworthy, Jérôme Loïcq, Benoît Seignovert, N. W. Kutsop et al.
Icarus
Astro and Planetary Science
article

Peculiar rainbows in Saturn’s E ring: Uncovering luminous bands near Enceladus

Matthew D. Kenworthy, Jérôme Loïcq, Benoît Seignovert, N. W. Kutsop, Stéphane Le Mouëlic, S. Cazaux, Niels Rubbrecht
article en

Abstract

We report observations of stripe-like features in Enceladus’ plumes captured simultaneously by Cassini’s VIMS-IR and ISS NAC instruments during flyby E17, with similar patterns seen in VIMS-IR data from flyby E13 and E19. These parallel stripes, inclined at approximately 16°to the ecliptic and 43°to Saturn’s ring plane, appear continuous across images when projected in the J2000 frame. A bright stripe, most visible at wavelengths around 5 μ m , acts as the zeroth-order diffraction peak of a reflection grating with an estimated groove spacing of 0.12–2.60 mm, while adjacent stripes are attributed to higher-order diffraction peaks. We suggest that this light-dispersing phenomenon originates from an inclined periodic structure within Saturn’s E ring. This structure, constrained between Saturn’s G-ring and Rhea’s orbit, likely consists of fresh ice particles supplied by Enceladus’ plumes. • Cassini’s ISS and VIMS uncover luminous, rainbow-like stripes near Enceladus. • Stripes show chromatic shifts, indicating diffraction by a millimetre-sized structure. • A bright band at 5 μ m lies at the centre of the stripe pattern. • Spectra hint at fresh, crystalline ice with large grains and solid CO 2 traces. • Discovery suggests an inclined, periodic ice formation in Saturn’s E ring.

IcarusVol. 441
Leiden University (NL), Centre National de la Recherche Scientifique (FR), Cornell University (US), Université Nantes Angers Le Mans (FR), Astronomy and Space (AU), Laboratoire de Planétologie et Géosciences (FR), Unité d'Appui et de Recherche OSUPS (FR), Delft University of Technology (NL)
Openalex Percentile: Top 92%
Astro and Planetary Science
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