Question

What are the various types of rainfall?Explain?

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Answer 1

Answer:

Originally based on the sources for the uplifting of the air, there are three main types of rainfall.

Originally based on the sources for the uplifting of the air, there are three main types of rainfall. 1. Convectional rainfall

Originally based on the sources for the uplifting of the air, there are three main types of rainfall. 1. Convectional rainfall2. Cyclonic/Frontal rainfall

Originally based on the sources for the uplifting of the air, there are three main types of rainfall. 1. Convectional rainfall2. Cyclonic/Frontal rainfall3. Orographic/Relief rainfall

Originally based on the sources for the uplifting of the air, there are three main types of rainfall. 1. Convectional rainfall2. Cyclonic/Frontal rainfall3. Orographic/Relief rainfallConvectional rainfall: It is typical of warm moist air by heating from the ground surface. As a result of heating of the surface air, the air expands and forced to rise to great height. As the air rises, it cools and becomes saturated and dew point temperature(the temperature at which water vapour in the air condense(gas-liquid)) is attained and then clouds will form. By further cooling, precipitation takes place

Originally based on the sources for the uplifting of the air, there are three main types of rainfall. 1. Convectional rainfall2. Cyclonic/Frontal rainfall3. Orographic/Relief rainfallConvectional rainfall: It is typical of warm moist air by heating from the ground surface. As a result of heating of the surface air, the air expands and forced to rise to great height. As the air rises, it cools and becomes saturated and dew point temperature(the temperature at which water vapour in the air condense(gas-liquid)) is attained and then clouds will form. By further cooling, precipitation takes placeNecessary conditions for Convective rainfall

Originally based on the sources for the uplifting of the air, there are three main types of rainfall. 1. Convectional rainfall2. Cyclonic/Frontal rainfall3. Orographic/Relief rainfallConvectional rainfall: It is typical of warm moist air by heating from the ground surface. As a result of heating of the surface air, the air expands and forced to rise to great height. As the air rises, it cools and becomes saturated and dew point temperature(the temperature at which water vapour in the air condense(gas-liquid)) is attained and then clouds will form. By further cooling, precipitation takes placeNecessary conditions for Convective rainfall1. Intense heating of the surface which causes the air to expand and rise.

Originally based on the sources for the uplifting of the air, there are three main types of rainfall. 1. Convectional rainfall2. Cyclonic/Frontal rainfall3. Orographic/Relief rainfallConvectional rainfall: It is typical of warm moist air by heating from the ground surface. As a result of heating of the surface air, the air expands and forced to rise to great height. As the air rises, it cools and becomes saturated and dew point temperature(the temperature at which water vapour in the air condense(gas-liquid)) is attained and then clouds will form. By further cooling, precipitation takes placeNecessary conditions for Convective rainfall1. Intense heating of the surface which causes the air to expand and rise.2. Abundant supply of moisture in the air to produce a very high relative humidity.

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Answer 2

Answer:

1. Conventional rainfall: Air naturally rises when it heats up, and it cools when it reaches higher elevations. Cool air can't hold as much moisture as warm air, so the moisture condenses into clouds known as cumulus clouds. 
2. Orographic rainfall: When moisture-laden air encounters a mountain range, the air is forced to rise. It cools off at the higher elevation, and this condenses water out of the air and creates rainfall. If the temperature is cold enough, the precipitation falls as snow.
3. Frontal rainfall: The meeting of a large mass of cold air and a large mass of warm air is called a front. The meeting creates turbulence. A frontal rain diagram can illustrate how the warm air rises over the cold air and forms large clouds when it cools, and moisture condenses. 
4. Monsoonal rainfall: The combination of the sun's heat and the Earth's rotation creates a band of easterly winds at 30 degrees north and south latitude. These winds blow all year, but they change direction with the seasons. 

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