Abstract
The Saturnian irregular satellite, Phoebe, can be broadly described as a
water-rich rock. This object, which presumably originated from the same
primordial population shared by the dynamically excited Kuiper Belt
Objects (KBOs), has received high-resolution spectral imaging during the
Cassini flyby. We present a new analysis of the Visual Infrared Mapping
Spectrometer observations of Phoebe, which critically, includes a
geometry correction routine that enables pixel-by-pixel mapping of
visible and infrared spectral cubes directly onto the Phoebe shape
model, even when an image exhibits significant trailing errors. The
result of our re-analysis is a successful match of 46 images, producing
spectral maps covering the majority of Phoebe’s surface, roughly a
third of which is imaged by high-resolution observations (
| Original language | English |
|---|---|
| Pages (from-to) | 23 |
| Journal | Astronomical Journal |
| Volume | 156 |
| Issue number | 1 |
| DOIs | |
| Publication status | Published - 22 Jun 2018 |
Keywords
- methods: data analysis
- planets and satellites: individual: Phoebe
- planets and satellites: surfaces