Adaptive optics (0.15 resolution) infrared images of the rings and satellites of Saturn were obtained in August 1995 as the Earth was crossing the ring plane. Twelve clumps were detected in the F ring, including HST S5 and S7 objects. For the first time H magnitudes were obtained for Prometheus, Pan
Keck Infrared Observations of Saturn's E and G Rings during Earth's 1995 Ring Plane Crossings
β Scribed by Imke de Pater; Mark R. Showalter; Jack J. Lissauer; James R. Graham
- Publisher
- Elsevier Science
- Year
- 1996
- Tongue
- English
- Weight
- 214 KB
- Volume
- 121
- Category
- Article
- ISSN
- 0019-1035
No coin nor oath required. For personal study only.
β¦ Synopsis
main rings are viewed edge-on and so reflect very little sunlight toward Earth. In this note, we discuss the first ground-based detection of Saturn's We report the first ground-based detection of Saturn's G G ring and the first infrared images of the E ring. ring, together with the first infrared images of the E ring. The 2. Observations and Results. We observed Saturn on UT 1995 May data were taken during the May and August 1995 ring plane 21-23 and 1995 August 9-11 using the 10-m W. M. Keck telescope crossings using the W. M. Keck telescope at a wavelength of on Mauna Kea, Hawaii. 1 We used the facility's near-infrared camera
2.26 m. The E ring's radial and vertical structure is found to (Matthews and Soiffer 1994), which is equipped with a Santa Barbara be generally consistent with previous results from Voyager and Research Corporation InSb array (256 by 256 pixels; the pixel size is Earth-based observatories; it has a brightness peak near the 0.151 arcsec). The observations were carried out with a narrow-band orbit of Enceladus and extends outward to Θ6 R S (Saturn radii). filter centered at a wavelength Ο 2.26 Θm (2.233-2.286 Θm), which The E ring is Θ40% fainter at 2.26 m than in the visual, falls in a methane absorption band. Sunlight, usually reflected by Saturn's thick cloud layers, is absorbed at this wavelength by methane gas above confirming and extending previous reports that it is very blue Saturn's cloud layers, making the planet very dark. The observations in color. The G ring is located at 2.8 R S and is unresolved in described in this note were taken on May 23, just after Earth's first vertical thickness. Its reflected intensity is similar to that found crossing of Saturn's ring plane, and on August 10, several hours before in the comparable Voyager image, implying that the ring is the second crossing. Thus the main rings were nearly edge-on, and the neutral in color from the visual to the infrared.
π SIMILAR VOLUMES
We analyze observations made in August and November 1995 during the Earth and Sun crossings of Saturn's ring plane, respectively. The August 1995 observations combine data taken with the Adonis adaptive optics system at the European Southern Observatory (ESO) and images from the Hubble Space Telesco