300
Mention 3 out of the 4 ways condensation cooling may be achieved.
Radiation cooling: The ground loses heat rapidly through terrestrial radiation and the air in contact with it is then cooled by conduction.
Advection cooling: Warm, moist air moves over a cooler and or sea surface.
Ortographic and frontal uplift: Warm, moist air is forced to rise either as it crosses a mountain barrieror when it meets a colder, denser mass of air at a front.
Convective/adiabatic cooling: Air is warmed in the daytime and rises in pockets as 'thermals'. As the air expands, it uses energy and so loses heat and the temperature drops. Because air is cooled by the reduction of pressure with height rather than loss of heat to the surrounding air, it is said to be adiabatically cooled.