To understand energy transfer during Sudden Stratospheric Warming (SSW) in the middle atmosphere, the 2023 SSW is studied by using the analysis tools of Multiscale Window Transform (MWT) and the MWT-based localized Energetics analysis and theory of Canonical Transfer (MS-ECT). The energy transfer in the mesosphere is diagnosed and compared with those in the stratosphere. The energy fields are first reconstructed onto three scale windows: large-scale window, SSW-scale window, and synoptic-scale window. Results show that the work done by pressure (pressure flux) plays a critical role in coupling the mesosphere and stratosphere during SSW events. The cross-scale energy transfer (canonical transfer) of available potential energy is always directed from the large-scale to the SSW-scale window, indicating the central role of baroclinic instability in both the stratosphere and mesosphere. Comparative analysis with the 2012/13 SSW event indicates consistent presence of baroclinic instability across both events, though the 2023 event exhibits significantly stronger energy transfer magnitudes in the mesosphere. These results highlight the consistent role of baroclinic instability and pressure flux in mediating cross-scale energy transfer during SSWs, providing a clearer understanding of stratosphere-mesosphere coupling.
Xiao-Qi et al. (Thu,) studied this question.