Retrievals of Jovian tropospheric phosphine from Cassini/CIRS

Icarus 172 (2004) 37-49

Authors:

PG Irwin, P. Parrish, T. Fouchet, S. B. Calcutt

Search for spatial variation in the jovian 15N/14N ratio from Cassini/CIRS observations

Icarus 172 (2004) 50-58

Authors:

SB Calcutt, Fouchet, Irwin, Parrish

Jupiter's atmospheric composition from the Cassini thermal infrared spectroscopy experiment.

Science 305:5690 (2004) 1582-1586

Authors:

VG Kunde, FM Flasar, DE Jennings, B Bézard, DF Strobel, BJ Conrath, CA Nixon, GL Bjoraker, PN Romani, RK Achterberg, AA Simon-Miller, P Irwin, JC Brasunas, JC Pearl, MD Smith, GS Orton, PJ Gierasch, LJ Spilker, RC Carlson, AA Mamoutkine, SB Calcutt, PL Read, FW Taylor, T Fouchet, P Parrish, A Barucci, R Courtin, A Coustenis, D Gautier, E Lellouch, A Marten, R Prangé, Y Biraud, C Ferrari, TC Owen, MM Abbas, RE Samuelson, F Raulin, P Ade, CJ Césarsky, KU Grossman, A Coradini

Abstract:

The Composite Infrared Spectrometer observed Jupiter in the thermal infrared during the swing-by of the Cassini spacecraft. Results include the detection of two new stratospheric species, the methyl radical and diacetylene, gaseous species present in the north and south auroral infrared hot spots; determination of the variations with latitude of acetylene and ethane, the latter a tracer of atmospheric motion; observations of unexpected spatial distributions of carbon dioxide and hydrogen cyanide, both considered to be products of comet Shoemaker-Levy 9 impacts; characterization of the morphology of the auroral infrared hot spot acetylene emission; and a new evaluation of the energetics of the northern auroral infrared hot spot.

Upper limits on hydrogen halides in Jupiter from Cassini/CIRS observations

Icarus 170:1 (2004) 237-241

Authors:

T Fouchet, G Orton, PGJ Irwin, SB Calcutt, CA Nixon

Abstract:

We have determined the following upper limits for the mole fraction of hydrogen halides in Jupiter's atmosphere from Cassini/CIRS observations: [HF] <2.7×10-11, [HCl] <2.3×10-9, [HBr]<1.0×10-9, [HI] <7.6×10-9. These limits are smaller than solar composition for HF and HCl, and support the halogens' condensation in ammonium salts predicted by thermochemical models for the upper jovian troposphere. © 2004 Published by Elsevier Inc.

High levels of atmospheric carbon dioxide necessary for the termination of global glaciation

Nature Springer Nature 429:6992 (2004) 646-649