DEW---when the ｔｅｍ p cools to its saturation point we call that dewpoint now to get the Word dew out of that we find that dew is what forms on the surface on grass and trees. FROZEN DEW---when the temp drops below freezing and then these dew particles turn into frozen water particles and collect on the surface as ice. particles and collect on the surface as ice. HAZE---will appear blue when you view it against a dark background/ and yellowish when you view it against A light background. FOG TYPES ACID FOG---fog that forms in a very polluted atmosphere can turn acidic and imposes great thereat to human RADIATION FOG---this is fog that is produced when the air cools this type forms best on clear and calm nights Also you have a shallow moist layer that forms near the surface and above that you have a dry layer. DRY AIR MOIST AIR SURFACE ADVECTION FOG---this fog forms when you cool surface air to its saturation point. Example bring in warm Moist air and move it over a very cool surface(heat is now transferred from the air to the surface) COLD OCEAN WARM MOIST AIR SURFACE A BC ABC BY VIEWING THE TEMP VS DEWPOINT FIND THE FOG

UPSLOPE FOG---this form of fog forms as it moist air flows upwards on an elevated plain or mountain. EVAPORATION FOG---this form of fog forms as it moist air flows upwards on an elevated plain or mountain.

CLOUDS(IN FEET) HIGH CLOUDS20,000-60,000 16,000-43,000 10,000-26,000 Cirrus(Ci) Cirrostratus(Cs) Cirrocumulus(Cc) MID CLOUDS6,500-26,000 6,500-23,0006,500-13,000 Altostratus(As) Altocumulus(Ac) LOW CLOUDS0-6, ,5000-6,500 Stratus(St) Stratocumulus(Sc) Nimbostratus(Ns) CLOUDS WITH VERTICAL DEVELOPMENTUNUSUAL CLOUDS Cumulus(Cu)Cumulonimbus(Cb)Lenticular Clouds/ Banner Cloud/ Pileus Mammatus/Nacreous/Noctilucent EQUATORUNITED STATESNORTH POLE