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New Model of the 15-micrometer Cooling of the Mesosphere and Lower Thermosphere

Alexander
Kutepov
The Catholic University of America
Abstract text

The year 2026 marks the 56th anniversary of Paul Crutzen’s (1995 Nobel Prize in Chemistry) hypothesis that collisions of CO₂ molecules with O(3P) atoms play a dominant role in the excitation of CO₂ in the mesosphere and lower thermosphere (MLT) and its 15-µm emission. The CO₂ + O(3P) problem has remained open for the past five decades due to unacceptably large discrepancies between (1) the small laboratory-measured rate coefficient, kO, estimated between (1.3–2.7) × 10−12 cm3 s−1 for this process, (2) the large kO ≃ (5-9) × 10−12 cm3 s−1 values inferred from space-based observations, and (3) the median kO = 3.0 × 10−12 cm3 s−1, routinely used in general circulation models (GCMs) to estimate CO₂ cooling of the MLT.
The current non-LTE models in CO₂ are inconsistent with observational facts. Using a large kO to fit the observed 15-µm signals contradicts the small, laboratory-confirmed kO. Using a small value for kO contradicts atmospheric observations. Using a median kO in current GCMs simultaneously contradicts both atmospheric observations and laboratory measurements.
We have proposed a new model for the non-LTE 15-µm cooling of the MLT, which is consistent with both laboratory experiments and space-based remote-sensing observations [1]. The model uses two different values for kO. First, the large value of kO = 6.0 × 10−12 cm3 s−1 is used to calculate the extent of CO₂ excitation that is consistent with the observed 15-µm emission. Second, the small, laboratory-established, kO = 1.5 × 10−12 cm3 s−1 is applied to determine the rate of energy exchange between the 15-µm radiation and the heat reservoir—the true CO₂ radiative cooling of the MLT.
We show that the standard non-LTE models, which utilize a single value for kO, strongly overestimate the total CO2 15-µm cooling of the MLT: for kO = 3.0 × 10−12 cm3 s−1, which is routinely applied in the GCMs, this excess radiative cooling can surpass 30 K/day. For kO = 6.0 × 10−12 cm3 s−1, the excess cooling reaches values up to 60 K/day.
Our results cast serious doubt on the widespread belief that the primary cooling mechanism of the MLT is the 15-µm infrared emission of CO₂. Other cooling mechanisms must compensate for the greatly reduced 15-µm cooling. One such mechanism is dynamical cooling, which involves the dissipation and/or breaking of gravity waves (GWs).

This research was supported by NSF (AGS-2312191/92, AGS-2125760, AGS-1301762) and NASA (80NSSC21K0664).

Kutepov, A.; Feofilov, A.; Rezac, L.; Kalogerakis, K.S. Remote Sensing in the 15-µm CO2 Band: Key Concepts and Implications for the Heat Balance of Mesosphere and Thermosphere. Remote Sens. 2025, 17, 1896. https://doi.org/10.3390/ rs17111896

Authors
Alexander Kutepov, The Catholic University of America
Artem Feofilov, Sorbonne University
Ladi Rezac, Max Planck Institute for Solar System Research
Konstantinos Kalogerakis, SRI International
Non-Student
Poster category
MLTS - Mesosphere or Lower Thermosphere General Studies
Poster number
2