Cassini CIRS and ISS opposition effects of Saturn’s rings – I. C ring narrow or broad surge?

Author:

Déau E12,Dones L3,Spilker L1,Flandes A4,Baillié K5,Pilorz S6,Showalter M6,El Moutamid M7,Colwell J E8

Affiliation:

1. NASA Jet Propulsion Laboratory, California Institute of Technology, Pasadena 91109 CA, USA

2. Department of Earth and Space Sciences, UCLA, Los Angeles 90095 CA, USA

3. SWRI, Southwest Research Institute, Boulder 80302 CO, USA

4. Departamento de Ciencias Espaciales, Instituto de Geofísica, Universidad Nacional Autónoma de México, Coyoacán 04510, Mexico City, México

5. IMCCE, Observatoire de Paris, Paris Sciences Lettres, CNRS, Sorbonne Universités, CNES, 75014 Paris, France

6. SETI Institute, Carl Sagan Center, Mountain View, 94043 CA, USA

7. Department of Astronomy, Center For Astrophysics and Planetary Sciences, Cornell University, Ithaca 14853 NY, USA

8. Department of Physics, UCF, Orlando, 32816 FL, USA

Abstract

Abstract We focus on the thermal and optical opposition effects of Saturn’s C ring seen by Cassini CIRS (Composite InfraRed Spectrometer) at 15.7 ${\mu}$m and ISS (Imaging Science Subsystem) at 0.6 ${\mu}$m. The opposition surge is a brightness peak observed at low phase angle (α → 0°). Saturn rings’ opposition surge was recently observed in reflected light and thermal infrared emission by Cassini. There is debate on whether the C ring’s thermal opposition surge width is narrow (≲1°) or broad (≳30°). This surge is important because its width was used to define the scale of ring properties driving the thermal peak. We parametrize the CIRS and ISS phase curves with several morphological models to fit the surge shape. For five of the largest C ring’s plateaus, we find that their thermal surge is 10 times wider than the optical surge and that the thermal surge width (∼4°) is neither narrow, nor broad. We compare radial differences between CIRS and ISS surge morphologies with the optical depth τ (from UVIS, UltraViolet Imaging Spectrograph) and water ice band depth (from VIMS, Visual and Infrared Mapping Spectrometer) profiles. We find that: water ice band depths (microscopic ring signatures) and τ (macroscopic ring signatures) show respectively little and large contrasts between the background and the plateaus. The thermal surge amplitude and τ are correlated, and we found no band depth dependence, contrary to the optical surge amplitude, which shows no correlation with τ. These correlations suggest a macroscopic scale dominance in controlling the C ring’s thermal opposition effect.

Funder

National Aeronautics and Space Administration

Jet Propulsion Laboratory

California Institute of Technology

PAPIIT

Publisher

Oxford University Press (OUP)

Subject

Space and Planetary Science,Astronomy and Astrophysics

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