A Composite of the Effects of Major Sudden Stratospheric Warming Events on Carbon Dioxide Radiative Cooling in the Mesosphere-Lower-Thermosphere

The major sudden stratospheric warming (SSW) events strongly influence the mean structure of the entire atmosphere, from the troposphere to the thermosphere. These events disrupt the compositional and thermal structure of the mesosphere and lower thermosphere (MLT), causing spatiotemporal variations in the concentration of trace species of this region. Currently, the role of dynamical changes during SSW events on radiative cooling in the MLT region is not well understood. An investigation of the SSW-induced changes in carbon dioxide (${\text{CO}}_2$) radiative cooling in the MLT region is presented by examining the changes in the dynamics and transport of key species, such as ${\text{CO}}_2$ and atomic oxygen (O). A composite analysis has been performed to understand these changes during the major SSW events that occurred between 2005 and 2020. The variation of trace species is found to be associated with the change in vertical residual circulation. The results also show that ${\text{CO}}_2$ radiative cooling decreases during the mesospheric cooling that occurs during the stratospheric warming over the polar region. During the recovery stage of the SSW event, the ${\text{CO}}_2$ radiative cooling enhances in the mesosphere. These variations in ${\text{CO}}_2$ radiative cooling are mainly caused by temperature perturbations and oxygen transport in the MLT region. The contribution of temperature change and transport have also been investigated in detail.