Abstract
New variables are introduced for a better thermodynamic representation of the air in the case we are interested in a wide to large scale or in sites at different altitudes above the average sea level or if we need to interpret weather maps for survey purposes. The parameters are equivalent temperature, potential temperature, equivalent-potential temperature and virtual temperature. The adiabatic, subadiabatic and superadiabatic gradients are also discussed in terms of atmospheric stability.
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