Temperature and composition of Saturn's polar hot spots and hexagon.
Science 319:5859 (2008) 79-81
Abstract:
Saturn's poles exhibit an unexpected symmetry in hot, cyclonic polar vortices, despite huge seasonal differences in solar flux. The cores of both vortices are depleted in phosphine gas, probably resulting from subsidence of air into the troposphere. The warm cores are present throughout the upper troposphere and stratosphere at both poles. The thermal structure associated with the marked hexagonal polar jet at 77 degrees N has been observed for the first time. Both the warm cyclonic belt at 79 degrees N and the cold anticyclonic zone at 75 degrees N exhibit the hexagonal structure.Isotopic ratios in titan's atmosphere from cassini CIRS limb sounding: CO2 at low and midlatitudes
Astrophysical Journal 681:2 PART 2 (2008) L101-L103
Abstract:
This Letter reports on a search for infrared emissions of isotopologues of COIsotopic ratios in titan's atmosphere from cassini cirs limb sounding: HC3N in the north
Astrophysical Journal 681:2 PART 2 (2008) L109-L111
Abstract:
This Letter reports the first detection of the three 13C isotopologues of HCA correlated-k model of radiative transfer in the near-infrared windows of Venus
JOURNAL OF QUANTITATIVE SPECTROSCOPY & RADIATIVE TRANSFER 109:6 (2008) 1118-1135
Condensation in Titan's stratosphere during polar winter
ICARUS 197:2 (2008) 572-578