The composition of the atmosphere of Jupiter

Chapter in Jupiter, Cambridge Univ Pr (2007)

Authors:

FW Taylor, SK Atreya, T Encrenaz, D Hunten, PG Irwin, TC Owen

Oxygen compounds in Titan's stratosphere as observed by Cassini CIRS

Icarus 186:2 (2007) 354-363

Authors:

FW Taylor, de Kok R, Irwin PGJ, Teanby NA

Vertical profiles of HCN, HC3N, and C2H2 in Titan's atmosphere derived from Cassini/CIRS data

Icarus 186 (2007) 364-384

Authors:

NA Teanby, P.G.J. Irwin, R. de Kok, S. Vinatier

Infrared observations of saturn and Titan from Cassini

Optics InfoBase Conference Papers (2007)

Authors:

DE Jennings, RK Achterberg, B Bézard, GL Bjoraker, JC Brasunas, R Carlson, A Coustenis, FM Flasar, PGJ Irwin, VG Kunde, AA Mamoutkine, CA Nixon, GS Orton, JC Pearl, PN Romani, ME Segura, AA Simon-Miller, EH Wishnow, S Vinatier

Abstract:

The Composite Infrared Spectrometer (CIRS) aboard the Cassini spacecraft has been orbiting Saturn for 2-1/2 years. CIRS is a Fourier transform spectrometer that measures atmospheric thermal structure and dynamics, and atmospheric composition, of Saturn and Titan. CIRS also maps the temperatures and dynamical processes of the rings and icy moons. © 2007 Optical Society of America.

Latitudinal variations in Uranus' vertical cloud structure from ukirt UIST observations

Astrophysical Journal 665:1 PART 2 (2007)

Authors:

PGJ Irwin, NA Teanby, GR Davis

Abstract:

Prior to Uranus' northern spring equinox in 2007 December, near-infrared spectra and images of Uranus were obtained in 2006 August and September using the UIST instrument on the United Kingdom Infrared Telescope (UKIRT). Latitudinally resolved spectra were recorded between 1 and 2.5 μm at a resolving power varying between 550 and 2000 with the instrument in long slit mode and with the slit aligned with the planet's central meridian to determine the north-south variations of Uranus' cloud structure. Our observations appear to be the first latitudinally resolved complete (1-2.5 μm) near-IR spectra of Uranus ever recorded, and we present initial determinations of the latitudinal variation of Uranus' vertical cloud structure from these data. We find two main cloud decks of similar density, one based near the 2 bar level and one based in the 8-10 bar region. The upper cloud is found to extend from 50° south to 45° north, increasing in thickness and altitude toward the south, especially in the south circumpolar collar at 45° south, but clearing toward the poles. However, we find that the deeper cloud layer is thickest at the equator and thins symmetrically toward both poles. We also report the firstever observation that the bright south circumpolar collar is, at some wavelengths, actually darker than other latitudes and provide an explanation of this phenomenon in terms of the latitudinal variations in cloud structure. © 2007. The American Astronomical Society.