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adiabatic advection air masses aloft altitude anticyclone appears atmosphere circulation clouds coast cold air cold front colder component condensation convection cooling cumulus curve decrease diagram direction distribution earth effects energy equation forecasting freezing geostrophic wind given ground heat height horizontal increase isallobars isentropic charts isentropic surfaces isobars isotherms lapse rate latitude layer lower mean meteorological moist moisture motion moving Northern Hemisphere observed obtained occur ocean Pacific particles polar potential temperature precipitation pressure gradient radiation rain region represented Rossby saturation shown in Fig slope snow specific humidity speed stations stratosphere stratus summer temperature inversion thunderstorms tion tropical air tropical cyclones tropopause troposphere trough turbulence U.S. Weather Bureau United unstable upper upper-air upward velocity vertical warm air warm front warmer water vapor wave wavelengths wedge westerlies winter