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Thermodynamics of the atmosphere
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air mass air parcel anticyclones atmosphere average boundary layer climate cloud droplets coefficient cold air component consider constant convective Coriolis force cyclones decreases with height diagram dry adiabat dry air earth earth's surface emagram enthalpy equation equilibrium flux density frontal function geopotential height geostrophic wind gradient ground heat horizontal hydrostatic equation ice particles image point increase intensive quantities isobaric surfaces large-scale motions latitudes liquid water meteorology mixing ratio moist air molecular molecules momentum motion systems non-saturated air perature plane planetary boundary layer polar front potential temperature precipitation pressure force radius regions relative humidity result rotation saturated air saturation adiabat saturation line scale sea level shown in Fig solar radiation specific humidity stable subtropical temperature-sounding curve thermal thermodynamic thermometer tion tropical troposphere turbulence unit mass unstable upper vector velocity vertical water vapor wavelength weather westerlies wet-bulb temperature wind speed