4.5 Article

Ray-tracing thermal modelling of Saturn's main rings

期刊

ICARUS
卷 354, 期 -, 页码 -

出版社

ACADEMIC PRESS INC ELSEVIER SCIENCE
DOI: 10.1016/j.icarus.2020.114063

关键词

Saturn main rings; Saturn rings' temperatures; Ray-tracing simulations

资金

  1. [DGAPA/PAPTIN105818]

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Observations by the Cassini spacecraft have provided new insights into our understanding of Saturn's rings, but there is still much unknown about the physical and thermal properties of the ring particles. This study focuses on reproducing the observed temperature profiles of the rings by considering their structural properties and energy sources, and evaluates different approaches to modeling the thermal behavior of the ring regions. The results suggest that slow rotators dominate and highlight the importance of shadowing effects for understanding the thermal characteristics of the rings.
The observations of the Cassini spacecraft gave new perspectives to our understanding of the rings of Saturn and their thermal studies due to their large variety of observation geometries. However, we still know little about the ring particles' physical and, particularly, thermal properties, which is the reason why a number of observations are not easy to explain. Nevertheless, the observed temperature profiles of the rings can be reproduced by considering the rings' general structural properties like local optical depth, z , and, for the optically-thick rings, wake properties like the ratios H/W or wake thickness to wake width, and H/W or wake separation to wake width; as well as their main energy input sources (e. g., direct and reflected solar energy and Saturn's infrared energy). In this work, we assume that the main rings (C, B, Cassini Division and A rings) are monolayers and study the temperature variations with solar elevation angle, B', of ten of their regions with a simple thermal balance equation that depends on the rings' shadowing behaviour due to the illumination geometry (B') and the arrangement of particles across the rings (tau). The shadowing is a key feature, which we reproduce with a numerical function obtained via ray tracing from arrays of spherical particles (C(B', tau)). Using the former model, we fit Cassini Composite Infrared Spectrometer (CIRS) temperature data with the Bond albedo, A v , and the so-called rotation parameter, f (which represents the rotation status of the ring particles) as only parameters. These parameters are two of the most important physical properties that define the rings' temperatures. With our method, we are able to reproduce the CIRS data temperature trends of the selected regions reasonably well. For evaluation purposes we compare the derived Bond albedo values with those obtained with the Cassini Imaging Science Subsystem (ISS) at wavelengths in the range 451 less than or similar to lambda less than or similar to 650 nm. The comparison suggests a dominance of slow rotators. Additionally, we evaluate the differences obtained when using either a numerical or an analytical shadowing function (in particular, that by (Altobelli et al., 2008)) in the thermal model. The differences between these two approaches reflect some details of the structure of the ring regions we study.

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