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air masses albedo altitude amount Antarctic anticyclones Arctic Arctic Ocean arid atmosphere average belt boundary cause circulation climate coast cold air continents cooling cumulus cyclones decrease direction earth earth's surface easterly effect energy equator equatorial evaporation figure flow global globe Greenland ground heat budget height high pressure areas high pressure cells higher latitudes horizontal humidity ice crystals increase intertropical convergence zone inversion jet stream land latent heat layers long-wave low pressure areas Ly/day maximum mean temperature meridional meteorological metres middle monsoon mountain movement North Northern Hemisphere occur oceans particles particularly period polar poles potential evaporation precipitation pressure gradient processes radiation balance rain rainfall reach regions result rise rotation seasonal showers silver iodide solar constant solar radiation Southern stratosphere subpolar subtropical high pressure summer thermal trade wind tropical tropopause troposphere unstable variations velocity vertical warm air water-vapour waves weather westerly winds winter