During winter the southern part of India receives highest rainfall also called the winter monsoon rainfall or retreating monsoon.
Delaware averages more inches of rainfall per year
There are so many things that are produced in India. Some of the common ones include medication drugs, chemicals, electronics, textiles and so much more.
The average rainfall during the monsoon season varies widely depending on the region, but in countries like India, it typically ranges from 500 to 1,500 millimeters (20 to 60 inches). The southwest monsoon, which usually lasts from June to September, accounts for a significant portion of the annual rainfall in these areas. Coastal regions often receive more rainfall compared to inland areas. Overall, monsoon rains are crucial for agriculture and water resources in many regions.
Tearfund, the UK christian relief and development agency has gone to and works in over fifty countries. Some of their more recent endeavors have been in Pakistan, India, Sudan, Haiti, Syria and Cambodia.
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.
Cherrapunji, Meghalaya has the highest rainfall rate in India. Recently a nearby village to Cherrapunji, ie., Mawsynram has been recording more rainfalls.
well because the rain is heavier and that make the mass wasting also known as mass movement is more common heavy when heavy rainfall
Because that part of our country receives more temp. & less rainfall........
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.
During winter the southern part of India receives highest rainfall also called the winter monsoon rainfall or retreating monsoon.
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.
After the rainfall it seems to be get a relief after a long and scorching heat of the summer, but in real after the dropping of one small water the earth became started heat releasing, and it will more significant if rain falls for a llittle amount. So, after the rainfall most of the cases the weather cool releasing its old humiliated warm.
Rather ironically, as Buddha was from India, Hinduism is far more common in India.
because jodhpur has lotitude of 53'25 whereas delhi is in 45"01
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.