Spectroscopic modeling study demonstrates collision-induced nitrogen absorption near 2.16 µm under terrestrial conditions, highlighting improved accuracy for atmospheric remote sensing.
Classical molecular dynamics simulations (CMDS) are used for calculations of the collision‐induced absorption (CIA) by pure N 2 in the (2.1–2.2 µm) region of the first overtone band. They lead to reasonable (±15%) agreement with the only two laboratory measurements available, at 97 K and room temperature. Based on these experiment/theory comparisons, empirical corrections are made to the CMDS‐calculated CIA of pure N 2 in the 200–300 K temperature range. In addition, the contribution of N 2 ‐O 2 collisions is, in the absence of any laboratory measurement, calculated and a simple semiempirical model (the first of its kind) is built in order to predict the CIA of N 2 under Earth atmosphere conditions. This is successfully validated by comparisons with ground‐based atmospheric transmission spectra in the 2.1–2.2 µm region.
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Hartmann et al. (2017) studied this question.
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