- 1High Altitude Observatory, NSF National Center for Atmospheric Research, Boulder, CO, USA.
- 2Laboratory for Atmospheric and Space Physics, University of Colorado, Boulder, CO, USA.
- 3Department of Mechanical, Materials, and Aerospace Engineering, Illinois Institute of Technology, Chicago, IL, USA.
We present analysis of the chemical and dynamical variability in the mesosphere and lower thermosphere (MLT) during the 2018-2019 sudden stratospheric warming (SSW) as simulated by the high resolution (~25 km horizontal and 0.1 scale height vertical resolution) version of the Whole Atmosphere Community Climate Model with thermosphere-ionosphere eXtension (WACCM-X). The WACCM-X simulations make use of new capabilities, including the spectral element dynamical core and the ability to constrain the lower atmosphere meteorology in WACCM-X at high-resolutions. Compared to standard resolution (~200 km horizontal and 0.25 scale height vertical resolution) WACCM-X simulations, the high-resolution simulations are in better agreement with Thermosphere Ionosphere Mesosphere Energetics Dynamics-Sounding of the Atmosphere using Broadband Emission Radiometry (TIMED-SABER) and Atmosphere Chemistry Experiment-Fourier Transform Spectrometer (ACE-FTS) observations. In particular, the high-resolution simulations better reproduce the Northern Hemisphere middle-high latitude winds in the MLT. The downward transport of nitric oxide (NO) following the SSW is also better reproduced in the high-resolution simulations. The results demonstrate the importance of capturing mesoscale processes for accurately simulating the chemistry and dynamics of the MLT.
How to cite: Pedatella, N., Harvey, V. L., Liu, H., and Datta-Barua, S.: High resolution simulations of the chemistry and dynamics in the mesosphere and lower thermosphere during the 2018-2019 sudden stratosphere warming, EGU General Assembly 2025, Vienna, Austria, 27 Apr–2 May 2025, EGU25-7273, https://doi.org/10.5194/egusphere-egu25-7273, 2025.