Publication Date:
2006-02-14
Description:
Observations were made and analyzed for Uranus, Saturn, and Titan in the continuum at the VLA and some spectroscopy at OVRO. Accurate A, B, C rings brightness temperatures from Saturn are a basis of scattering theory calculations. Variations of 2 cm limb darkening with pole orientation were modeled and are shown to originate in the deep atmosphere.
Keywords:
ASTRONOMY
Type:
NASA, Washington Reports of Planetary Astronomy, 1985; p 47-48
Format:
text