Interferometric observations of the atmosphere of Titan were performed with the Submillimeter Array on two nights in February 2004 to investigate the global average vertical distributions of several molecular species above the tropopause .
Rotational transitions of CO , isomers of HCN , and HC _ { 3 } N were simultaneously recorded .
The abundance of CO is determined to be 51 \pm 4 ppm , constant with altitude .
The vertical profile of HCN is dependent upon the assumed temperature but generally increases from 30 ppb at the condensation altitude ( \sim 83 km ) to 5 ppm at \sim 300 km .
Further , the central core of the HCN emission is strong and can be reproduced only if the upper stratospheric temperature increases with altitude .
The isotopic ratios are determined to be ^ { 12 } C/ ^ { 13 } C=132 \pm 25 and ^ { 14 } N/ ^ { 15 } N=94 \pm 13 assuming the Coustenis & Bézard ( 1995 ) temperature profile .
If the Lellouch ( 1990 ) temperature profile is assumed the ratios decrease to ^ { 12 } C/ ^ { 13 } C=108 \pm 20 and ^ { 14 } N/ ^ { 15 } N=72 \pm 9 .
The vertical profile of HC _ { 3 } N is consistent with that derived by Marten et al .
( 2002 ) .