Given the fact that plots of Troposphere Tricellular Circulation are only based on weather mean conditions measured near the ground (i.e.: pressure and wind fields observed at the surface of the Earth), we want to improve the plots of streamlines of the general circulation of the troposphere, by using the impacts of thermoelastic properties of saturated water vapor on atmosphere vertical motions. Our results are based on Mbanes’ equation of Atmosphere dynamic balance which shows precisely that, unlike the dry water vapor that can be assimilated to the ideal gas at all circumstances, the saturated water vapor has, in an air parcel at the same time very cold (temperatures below 0.0098° C) and rich in moisture (vapor pressure above 6.11 mb), thermoelastic properties diametrically opposed to those of ideal gas (including dry water vapor). Vertical profiles of temperature and water vapor in the troposphere (provided by ground-or space-based observations) lead to the location of the air parcel in which the ideal gas assumption should be banned; hence the appropriate plots of troposphere tricellular circulation streamlines.
