Laboratory measurements of the quenching of CO 2 ( ν 2 ) by O atoms are presented over the 142–490 K temperature range relevant to the 75–120 km altitude region of the terrestrial atmosphere. The primary cooling mechanism in this region occurs when CO 2 is efficiently excited through collisions with ambient O atoms, populating the bending vibrational ( ν 2 ) modes. A significant fraction of the vibrationally excited CO 2 relaxes through spontaneous 15‐ μ m emission that escapes into space, thereby removing kinetic energy from this region of the atmosphere and generating a local cooling effect. The rate coefficient for the vibrational relaxation of CO 2 ( ν 2 ) by O atoms, k O ( ν 2 ), is measured using transient diode laser absorption spectroscopy. A slight negative temperature dependence is observed for k O ( ν 2 ), with values ranging from 2.7 (±0.4) × 10 −12 cm 3 s −1 at 142 K to 1.3 (±0.2) × 10 −12 cm 3 s −1 at 490 K.
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Castle et al. (2012) studied this question.
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