Question

explain the forms of condensation in detail.

Answer 1

"Giving out" > the air itself has not reached its dew-point, and no floating dew is visible.  Only air that touches a cold surface, shrinks, reaches its dew point, and leaves behind water.  All plants in deserts live and survive using this process; and in moderate climates, plants survive periods of drought by using the 'giving out' phenomenon. The Groasis Waterboxx plantcocoon® copies this process;

Dew > only the lowest part of air above the soil, in the lowest point of a valley, or in a canal, reaches the dew point.  In general, we see beautiful horizontal layers of dew;

High humidity > the whole mass of air is slightly saturated, but visibility is still OK;

Mist > the whole air is heavily saturated with water, and visibility is bad;

Clouds around mountain tops > warm air rising against the slope gets colder, reaches its dew point, and shows itself as clouds;

Clouds > close to Earth it's warm enough to avoid the dew point; but higher up, it's colder and clouds develop.

3 types of precipitation:

Floating water molecules bind to each other (cohesion) and become too heavy to float.  When they fall, we call this ‘rain’;

Floating water molecules bind to each other, freeze into irregular lumps of ice, and become too heavy to float.  When they fall, we call this ‘hail’;

Floating water molecules bind to each other, become crystalline water (i.e. ice) too heavy to float.  When they fall, we call this ‘snow’. 

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