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convectional relief is formed with the formation of convectional currents. the surface of the earth is heated and the air above it aswell. the air mass expands and becomes lighter. but as the airmass rises it cools. it continues to rise till it reaches due point. condensation occurs, clouds are formed. previpitation results. cyclonic precipitation results when the leading edge of the warm air mass meets a cool air mass. the warm air mass rises above the cool air mass. it cools adiabatically. the moisture condenses, clouds are formed, precipitation results.

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Convectional and orographic are?

Convectional and orographic are types of rainfall. Convectional rainfall occurs when the ground is heated, causing warm air to rise and form cumulonimbus clouds that can result in localized heavy downpours. Orographic rainfall happens when moist air is forced to rise over mountain ranges, leading to cooling, condensation, and precipitation on the windward side of the mountains.


How does convectional rainfall relief rainfall and frontal rainfall occur?

Convectional rainfall occurs when warm air rises, cools, and condenses to form rain clouds. Relief rainfall occurs when moist air is forced to rise over elevated terrain and cool, leading to precipitation. Frontal rainfall occurs when two air masses with different temperatures and moisture content meet, causing the warmer air to rise and condense, resulting in rainfall.


What types of rainfall are there?

The main types of rainfall are convective, frontal, orographic, and cyclonic. Convective rainfall occurs when warm air rises and cools, leading to condensation and precipitation. Frontal rainfall happens when two air masses with different temperatures meet, causing the warm air to rise and cool. Orographic rainfall occurs when moist air is forced to rise over a mountain range, cooling and creating precipitation. Cyclonic rainfall results from the convergence of air masses around a low-pressure system, leading to widespread precipitation.


What are the factors responsible for relief rainfall?

The factors are moist air and rainfall.


The difference in elevation between the highest and lowest parts of an area?

The difference in elevation between the highest and lowest points of an area is known as the relief. It is a measure of the variation in height within a specific region, often used to describe the topography or terrain of a landscape. High relief indicates steep slopes or large variations in elevation, while low relief suggests flatter terrain.

Related Questions

What are the types of rainfall?

relief rainfall convectional rainfall Frontal rainfall


What are the 3 types of rainfall?

Some fancy names have been given to this question, Convectional, Orographic and Frontal. I will stick to the more simple types such as Lite falls , mediums falls and heavy or flooding rains. I am also including mist and fog because they both contain water vapour.


Convectional and orographic are?

Convectional and orographic are types of rainfall. Convectional rainfall occurs when the ground is heated, causing warm air to rise and form cumulonimbus clouds that can result in localized heavy downpours. Orographic rainfall happens when moist air is forced to rise over mountain ranges, leading to cooling, condensation, and precipitation on the windward side of the mountains.


What is relief convectional?

Relief convectional refers to a type of rainfall that occurs when moist air is forced to rise over a barrier such as a mountain range, leading to cooling and condensation. This process forms clouds and eventually results in precipitation on the windward side of the barrier.


How does convectional rainfall relief rainfall and frontal rainfall occur?

Convectional rainfall occurs when warm air rises, cools, and condenses to form rain clouds. Relief rainfall occurs when moist air is forced to rise over elevated terrain and cool, leading to precipitation. Frontal rainfall occurs when two air masses with different temperatures and moisture content meet, causing the warmer air to rise and condense, resulting in rainfall.


What are the three types of convectional rainfall?

The three main types of rainfall are: convectional rainfall, relief rainfall and frontal rainfall. Relief rainfall is when the warm moist air from the sea ( Atlantic Ocean) is forced to rise over mountains and as the moist air gets higher it gets colder so it gradually condenses and becomes water droplets and it rains/ prcipitates. Relief rainfall is common along the west side of Britain where there are more high lands. Convectional rainfall is when the sun comes out and heats up the land, this causes the air around it to become warm too. The warm air currents rise and as it rises it gets colder so it gradually condenses and the water vapou become water droplets and it rains/precipitates. Convectional rainfall is mostly common around towards the south of Britain in the summer. Frontal rainfall is when cold air and warm air meet, the warm, light air wants to get past the heavy cold air so it casually rises above it. Its rising makes it get colder which makes the warm air cold air, so it condenses and becomes rain/ precipitation! Frontal rainfall is mostly common all over Britain especially in the winter.


What types of rainfall are there?

The main types of rainfall are convective, frontal, orographic, and cyclonic. Convective rainfall occurs when warm air rises and cools, leading to condensation and precipitation. Frontal rainfall happens when two air masses with different temperatures meet, causing the warm air to rise and cool. Orographic rainfall occurs when moist air is forced to rise over a mountain range, cooling and creating precipitation. Cyclonic rainfall results from the convergence of air masses around a low-pressure system, leading to widespread precipitation.


What is the Difference between normal relief and high relief coin?

what is differenc between high relief and normal relief


What is the explanation for the three types of rainfall?

The three main types of rainfall are: convectional rainfall, relief rainfall and frontal rainfall. Relief rainfall is when the warm moist air from the sea (Atlantic Ocean) is forced to rise over mountains and as the moist air gets higher it gets colder so it gradually condenses and becomes water droplets and it rains/ prcipitates. Relief rainfall is common along the west side of Britain where there are more high lands. Convectional rainfall is when the sun comes out and heats up the land, this causes the air around it to become warm too. The warm air currents rise and as it rises it gets colder so it gradually condenses and the water vapou become water droplets and it rains/precipitates. Convectional rainfall is mostly common around towards the south of Britain in the summer. Frontal rainfall is when cold air and warm air meet, the warm, light air wants to get past the heavy cold air so it casually rises above it. Its rising makes it get colder which makes the warm air cold air, so it condenses and becomes rain/ precipitation! Frontal rainfall is mostly common all over Britain especially in the winter.


What is the difference between high relief and low relief?

The difference between high relief and low relief is that high relief has more depth and low relief is more casual and not as 3D. In high relief, it's much closer to 3D.


Why relief rainfall is more common in India and why?

in india most of the rainfall is relief rainfall


What are the types of rainfall in Ghana?

relief rainfall, cyclonic rainfall