The factors are moist air and rainfall.
Relief rain is when moist air from the sea rises over a mountain and the air gets cold and forms clouds and the rain mostly falls on one side and becomes less at the bottom
Relief precipitation is when an air mass rises to cross a mountain barrier. It is also called Orthographic Precipitation.
types of rainfall. orographic is commonly called relief rainfall.
there are 3 types of rainfall which are still exsisting: relief rainfall convectional rainfall Frontal rainfall
The factors are moist air and rainfall.
Relief rainfall occurs when moist air is forced to rise over a physical barrier such as a mountain or tall buildings. As the warm, moist air rises over the mountain, it cools and the water vapour condenses, forming rain. Ta-daa!! Lol. On the side of the barrier with the rising air, rainfall occurs, but little or no rainfall occurs on the other side. This area of little or no rainfall is called the rainshadow area. Relief in general deals with the height of the land. :)
There are three main types of rainfall, 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. Convestional 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, it condenses and guess what? It rains/ precipitates! Frontal rainfall is mostly common all over Britain especially in the winter.
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.
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.
daigram of a relief rainfall
relief rainfall convectional rainfall Frontal rainfall
in india most of the rainfall is relief rainfall
Convectional rainfall is caused when heating on the Earth's surface cause air to rise. The air cools as it rises and condensates into rain.
they can't act as air barriers because they have large air space between them
Relief rainfall
relief rainfall, cyclonic rainfall