CONDENSATION AND ASSOCIATED FORMS The

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CONDENSATION AND ASSOCIATED FORMS The transformation of gaseous form of water (i.e. water vapour) into solid form (ice) and liquid from (water) is called condensation. In other words, the process of change of water vapour into liquid form

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CONDENSATION AND ASSOCIATED FORMS<br>
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The transformation of gaseous form of water (i.e. water vapour) into solid form (ice) and liquid from (water) is called condensation.
In other words, the process of change of water vapour into liquid form is called condensation.
The process and mechanism of condensation depends on the amount of relative humidity present in the air.
The air having 100% relative humidity is called saturated air. An air may become saturated in two ways e.g. either (1) the absolute humidity at a given temperature is raised to equal the humidity retaining capacity of the air or (2) The temperature of the air is reduced to such an extent that the humidity capacity becomes equal to its absolute humidity.<br>
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The temperature at which an air becomes saturated is called dew point. It may be pointed out that condensation will begin only when the air is supersaturated e.g. if the relative humidity exceeds 100 percent, and this can be achieved only when the air is further cooled.
If dew point is above freezing point (32°F), condensation will occur in liquid form (e.g., dew, fog, rainfall etc.) but if dew point is below freezing point, condensation occurs in solid form (e.g., frost, ice, snow, hailstorm etc.).
It is apparent that condensation depends on (1) the percentage of relative humidity of the air and (2) the degree of cooling of the air. The air becomes cool when it rise while it gets heated when it descends.
Thus, the ascending air may bring moist weather while descending air causes dry condition.<br>