The geometric albedos of Uranus and Neptune between 2100 and 3350 A

Physics – Optics

Scientific paper

Rate now

  [ 0.00 ] – not rated yet Voters 0   Comments 0

Details

16

Albedo, Neptune (Planet), Planetary Atmospheres, Ultraviolet Astronomy, Uranus (Planet), Atmospheric Optics, Atmospheric Scattering, Line Spectra, Reference Stars

Scientific paper

Results are reported from large aperture IUE observations of the stratospheres of Uranus and Neptune. The data were collected using 16 Cyg A and B as solar analog stars. The spectra observed were similar to geometric albedos of the predicted in terms of Rayleigh-Raman scattering in the 2200-2800 A region. A falloff was observed near visible wavelengths, a factor which might be attributable to low-altitude haze absorbing in the 3000-4000 A interval. The data also indicated that the Uranus stratosphere does not strongly absorb UV radiation, and is not a good heating source. The stratospheric haze constituents over Uranus could therefore be condensates of CH4 and H2 photochemistry.

No associations

LandOfFree

Say what you really think

Search LandOfFree.com for scientists and scientific papers. Rate them and share your experience with other people.

Rating

The geometric albedos of Uranus and Neptune between 2100 and 3350 A does not yet have a rating. At this time, there are no reviews or comments for this scientific paper.

If you have personal experience with The geometric albedos of Uranus and Neptune between 2100 and 3350 A, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and The geometric albedos of Uranus and Neptune between 2100 and 3350 A will most certainly appreciate the feedback.

Rate now

     

Profile ID: LFWR-SCP-O-893179

  Search
All data on this website is collected from public sources. Our data reflects the most accurate information available at the time of publication.