The lower thermosphere during the northern hemisphere winter of 2009: A modeling study using high-altitude data assimilation products in WACCM-X

We present numerical simulations using the Whole Atmosphere Community Climate Model, extended version, constrained below 90km by a combination of NASA's Modern Era Retrospective Analysis for Research and Applications and the U.S. Navy's Operational Global Atmospheric Prediction System - Advanced Level Physics High Altitude assimilation products. The period examined is January and February 2009, when a large stratospheric warming occurred on 24 January 2009, with anomalous circulation persisting for several weeks after the event.

In this study, we focus on the dynamical response of the lower thermosphere up to 200km. We find evidence of migrating and nonmigrating tides, Rossby and Rossby-gravity modes, and Kelvin waves, whose amplitudes appear to be modulated at the times leading and following the stratospheric warming. While the Rossby, Rossby-gravity, and Kelvin modes are rapidly dissipated in the lower thermosphere (above 110km), the tides maintain substantial amplitude throughout the thermosphere, but their vertical structure becomes external above about 120-150km.