Water In The Atmosphere
Following are the characteristics of the zonal distribution of relative humidity:
i. It is the highest at the equator and decreases towards poles.
ii. It is minimum in subtropical regions.
iii. It increases from 30°, north and south towards poles, because of the decrease in temperature.
iv. The belt of relative humidity shifts north and southwards with the annual movement of the sun.
Sponsor Area
Sponsor Area
Sponsor Area