T. Encrenaz et al., ISO OBSERVATIONS OF URANUS - THE STRATOSPHERIC DISTRIBUTION OF C2H2 AND THE EDDY DIFFUSION-COEFFICIENT, Astronomy and astrophysics, 333(2), 1998, pp. 43-46
The infrared spectrum of Uranus has been recorded between 7 and 16.5 m
u m with the grating mode of the Short-Wavelength Spectrometer of ISO,
with a resolving power of 1500. The 6-12 mu m spectrum of Uranus has
also been recorded at lower resolution (R=90) by the PHOT instrument i
n spectroscopic mode. The spectra show no signatures other than the C2
H2 band centered at 13.7 mu m. From the absence of emission in the reg
ion of the CH4 7.7 mu m band, and by fitting the C2H2 data on the basi
s of a photochemical model, the eddy diffusion coefficient is retrieve
d (in the range 5 10(3)-10(4) cm(2) s(-1) at the homopause). This resu
lt is consistent with the values previously derived from the Voyager U
V occultation experiments.