They can be of various types depending upon the process of precipitation, obstacles etc.
Convectional Rain
The, air on being heated, becomes light and rises up in convection currents. As it rises, it expands and loses heat and consequently, condensation takes place and cumulous clouds are formed. With thunder and lightening, heavy rainfall takes place but this does not last long. Such rain is common in the summer or in the hotter part of the day. It is very common in the equatorial regions and interior parts of the continents, particularly in the northern hemisphere. Whenever there is an ascending mass of air, it leads to more rain, whenever the air descends, it leads to lower rains.
Orographic Rain
When the saturated air mass comes across a mountain, it is forced to ascend and as it rises, it expands; the temperature falls, and the moisture is condensed. The chief characteristic of this sort of rain is that the windward slopes receive greater rainfall. After giving rain on the windward side, when these winds reach the other slope, they descend, and their temperature rises. Then their capacity to take in moisture increases and hence, these leeward slopes remain rainless and dry. The area situated on the leeward side, which gets less rainfall is known as the rain-shadow area. It is also known as the relief rain.
Cyclonic Rain
As in case of tropical and extra tropical cyclones.
GPSC Notes brings Prelims and Mains programs for GPSC Prelims and GPSC Mains Exam preparation. Various Programs initiated by GPSC Notes are as follows:-
- GPSC Mains 2024 Tests and Notes Program
- GPSC Prelims Exam 2024- Test Series and Notes Program
- GPSC Prelims and Mains 2024 Tests Series and Notes Program
- GPSC Detailed Complete Prelims Notes