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This result cannot be explained by the present model atmosphere and one possible explanation is the contribution by the emission of CO and CS in the outer atmosphere.
Therefore, the vertical distribution of ozone VMR can be retrieved from the observed emission line shape by means of radiative transfer in a model atmosphere and an optimal estimation method.
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It should be pointed out that this variation, controlling the entire ocean area where the ACC resides, represents one dominant meteorological signal that is actually not captured by the present atmosphere ocean general circulation models (Atmosphere and Ocean De-aliasing Level-1B products adopted by the GRACE project to yield the GAD data and removed from the GRACE observations as stated).
In the processing of recorded data, we first subtract the Doppler shift calculated from the orbital information and a model atmosphere from the original signal by heterodyning, thereby suppressing the frequency variation and enabling narrow-band filtering.
Synthetic spectra were calculated by means of line-by-line method using the HITRAN 2004 molecular database (Rothman et al, 2005) and the CO2 HITEMP database (Wattson and Rothman, 1992; Pollack et al., 1993), the VIRA1985 model atmosphere (Keating et al., 1985), and a solar line atlas (Livingston and Wallace, 1991).
The linear growth rates of the Rayleigh-Taylor (R-T) instability in the ionosphere from 2011 to 2013 were obtained with a whole atmosphere-ionosphere coupled model GAIA (ground-to-topside model of atmosphere and ionosphere for aeronomy).
The model atmosphere extended from the surface to 70 km and had the starting composition, pressure and temperature of the 1976 US Standard Atmosphere.
The thermosphere wind and temperature parameters are obtained from Ground-to-topside model of Atmosphere and Ionosphere for Aeronomy (GAIA) model simulations.
The behavior of three steels (P92, T22 and SANICRO 28) and several coatings in the above described biomass model atmosphere is compared.
The mesosphere wind reversal is also noticed in "Specified Dynamics" version of Whole Atmosphere Community Climate Model (SD-WACCM) and Ground-to-topside model of Atmosphere and Ionosphere for Aeronomy (GAIA) simulations.
The initial thermodynamic structure of the unperturbed model atmosphere is defined by moist adiabatic lapse rate up to 17 km and a constant temperature above this height.
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