During major sudden stratospheric warmings, mesosphere-lower-thermosphere CO2 radiative cooling decreases by roughly 35 percent and later increases by roughly 25 percent, driven mainly by temperature and atomic oxygen transport.
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A composite of the effects of major sudden stratospheric warming events on carbon dioxide radiative cooling in the mesosphere-lower-thermosphere
During major sudden stratospheric warmings, mesosphere-lower-thermosphere CO2 radiative cooling decreases by roughly 35 percent and later increases by roughly 25 percent, driven mainly by temperature and atomic oxygen transport.