Cd. Parkinson et al., Estimates of atomic deuterium abundance and Lyman-alpha airglow in the thermosphere of Jupiter, GEOPHYS R L, 26(20), 1999, pp. 3177-3180
We have made calculations of the atomic D distribution in the thermosphere
of Jupiter. The principal reactions determining the D abundance appear to b
e generation by reaction of H with vibrationally hot HD and loss by reactio
n of D with H-2(v=0,1) and CH3. The H and CH3 distributions have been calcu
lated using a 1-D photochemical-diffusion model with the column H constrain
ed using the Lyman-alpha airglow. For H-2 effective vibrational temperature
s, T-v, between 1 and 4 times kinetic we find D columns between 4 x 10(11)
and 2 x 10(13) atoms cm(-2). HD can be vibrationally excited due to VV ener
gy transfer from H-2(v=1). Using a radiative transfer model with coupling o
f the H and D Lyman-alpha lines we have calculated line profiles and total
intensities across the Jovian disk and on the limb. For the above D columns
and a H column similar to 3.5 x 10(17) cm(-2), compatible with equatorial
Lyman-alpha airglow observations, the disk D intensity varies from 80 to 60
0 R for overhead Sun and viewing, whereas on the terminator the D maximum t
otal intensity is similar to 60 R at similar to 860 km above the 1 bar leve
l for the maximum D column.