Ionosphere and Upper Atmosphere
Thermosphere extension of the Whole Atmosphere Community Climate Model
Article first published online: 4 DEC 2010
DOI: 10.1029/2010JA015586
Copyright 2010 by the American Geophysical Union.
Issue
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Journal of Geophysical Research: Space Physics (1978–2012)
Volume 115, Issue A12, December 2010
Additional Information
How to Cite
, et al. (2010), Thermosphere extension of the Whole Atmosphere Community Climate Model, J. Geophys. Res., 115, A12302, doi:10.1029/2010JA015586.
Publication History
- Issue published online: 4 DEC 2010
- Article first published online: 4 DEC 2010
- Manuscript Accepted: 3 SEP 2010
- Manuscript Revised: 5 AUG 2010
- Manuscript Received: 20 APR 2010
Keywords:
- whole atmosphere;
- thermosphere;
- global circulation model;
- atmosphere coupling;
- planetary waves and tides
[1] In atmospheric and space environment studies it is key to understand and to quantify the coupling of atmospheric regions and the solar impacts on the whole atmosphere system. There is thus a need for a numerical model that encompasses the whole atmosphere and can self-consistently simulate the dynamic, physical, chemical, radiative, and electrodynamic processes that are important for the Sun-Earth system. This is the goal for developing the National Center for Atmospheric Research (NCAR) Whole Atmosphere Community Climate Model (WACCM). In this work, we report the development and preliminary validation of the thermospheric extension of WACCM (WACCM-X), which extends from the Earth's surface to the upper thermosphere. The WACCM-X uses the finite volume dynamical core from the NCAR Community Atmosphere Model and includes an interactive chemistry module resolving most known neutral chemistry and major ion chemistry in the middle and upper atmosphere, and photolysis and photoionization. Upper atmosphere processes, such as nonlocal thermodynamic equilibrium, radiative transfer, auroral processes, ion drag, and molecular diffusion of major and minor species, have been included in the model. We evaluate the model performance by examining the quantities essential for the climate and weather of the upper atmosphere: the mean compositional, thermal, and wind structures from the troposphere to the upper thermosphere and their variability on interannual, seasonal, and daily scales. These quantities are compared with observational and previous model results.

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