The comparative approach to planetary problems is becoming increasingl
y fruitful as new information from various planet atmospheres is assim
ilated. In particular, it is clear that the important problem of CO2 c
ooling in the Earth's lower thermosphere is closely tied to the thermo
spheric heat budgets of Venus and Mars. CO2 cooling in each of these t
hermospheres is strongly impacted by collisions of CO2 and O, yielding
vibrationally excited CO2 and enhanced 15-mum emissions in regions wh
ere non-local thermodynamic equilibrium conditions prevail. Both the r
elative abundance of atomic O and the CO2-O relaxation rate affect the
magnitude of this enhanced cooling process. We examine the recent pro
gress in the debate on the CO2-O relaxation rate, its temperature depe
ndence, and its corresponding impact on the thermospheric heat budgets
of Venus, Earth, and Mars. This comparative approach provides the bro
adest range of conditions under which a common CO2-O relaxation mte sh
ould provide consistent results. New global mean calculations are pres
ented for the heat budgets of these three planets using large CO2-O re
laxation rates that have been inferred recently from Earth CO2 radianc
e measurements and laboratory studies. Results indicate that available
Venus and Mars data constrain the CO2-O relaxation rate to be 2-4 x 1
0(-12) cm3/s at 300 K. For Venus, this strong cooling serves as an eff
ective thermostat that gives rise to a small variation of thermospheri
c temperatures over the solar cycle, just as observed. Conversely, CO2
cooling does not appear to be dominant in the dayside heat budget of
the Mars thermosphere over most of the solar cycle. For the Earth, thi
s strong cooling implies that the lower thermosphere does not typicall
y require significant eddy diffusion or heat conduction. However, glob
al-scale dynamics or an additional heating mechanism may be needed to
restore calculated temperatures to observed values when relaxation rat
es exceeding 2 x 10(-12) cm3/s are employed.