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Three parametric models proposed in the bibliography are compared and calibrated, and a new model is proposed to account for the alternation of vertical atmosphere profile by clouds.
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The atmosphere of Jupiter has a strong vertical air circulation, which would carry these compounds down into the lower regions.
Magnitudes of CO2, CH4 and N2O sources and sinks are defined as the vertical land-atmosphere exchanges.
Clear signatures of the interaction between enhanced PWs and tides during SSW and the resulting influence on the upper atmospheric EEJ strength and TEC values are presented to demonstrate the vertical coupling of atmospheres and its dependence on solar activity and planetary wave activity in the lower atmosphere.
Using two independently measured upper atmospheric parameters, namely the EEJ and the TEC, the vertical coupling of atmospheres during SSW events at varying levels of solar activity has been investigated.
This study thus provides experimental evidence to the conjecture proposed earlier and revealed new aspects of interactions on the vertical coupling of atmospheres.
Laskar et al. (2014) studied vertical coupling of atmospheres depending on the strength of sudden stratospheric warming (SSW) and solar activity.
These results suggest that the vertical coupling of atmospheres is stronger during strong major SSW events and these events play an important role in enabling the coupling even during high solar activity.
To conclude, the vertical coupling of atmospheres in terms of the strength of spectral amplitude is found to be dependent on the strength of SSW, solar activity, and interaction between tides and planetary waves.
The authors concluded that the vertical coupling of atmospheres in terms of the strength of the spectral amplitude was found to be dependent on the strength of SSW, the solar activity, and the interaction between tides and planetary waves.
Atmospheric conditions such as vertical and horizontal temperature, atmosphere pressure, wind speed, and water vapor density are mostly responsible for PM2.5 dispersion (i.e., the sinks) (Liu 1985; Janhäll 2015; Rohde and Muller 2015).
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