Flub136 I do not think this a true representation of the warming
An important character of sudden warming is its downward propagation from 45 km into the lower stratosphere. This feature is not zonal in character, but has nonzonal structure, with a planetary wave tilting westward with height. In the middle latitudes, warming in the stratosphere (40 km) is followed by cooling in the mesosphere (65 km). Simultaneously, the opposite occurs in low latitudes, with stratospheric cooling and mesospheric warming, but the magnitude of the changes in the lower latitudes is one order less compared to that noted in higher latitudes