it damages everything and no one can relate to anything because the rainfall is dried out
Rainfall significantly influences population patterns in South Asia by affecting agriculture, water availability, and overall living conditions. Areas with consistent and adequate rainfall, such as the Indo-Gangetic Plain, tend to support higher population densities due to fertile land and agricultural productivity. Conversely, regions with low or erratic rainfall, like parts of Western India and Pakistan, often experience lower population densities and higher rates of migration towards more hospitable areas. Additionally, seasonal monsoons play a critical role in shaping settlement patterns and economic activities across the region.
Countries north of the equator with slight or moderate rainfall include Mexico, Egypt, and Saudi Arabia. Countries south of the equator with similar rainfall patterns include Australia, Chile, and South Africa.
South America has diverse climates with varying rainfall patterns across different regions. The Amazon rainforest, for example, receives high annual rainfall levels, while coastal desert areas like the Atacama Desert in Chile are extremely dry. The overall rainfall in South America can range from very high in tropical regions to very low in desert areas.
South Carolina's average rainfall is 51 inches a year South Carolina's average rainfall is 51 inches a year South Carolina's average rainfall is 51 inches a year South Carolina's average rainfall is 51 inches a year
Rainfall patterns of South Sahara favored locally domesticated grains rather than wheat and barley.
The average annual rainfall for South Australia is 236mm. A large area of the state is extremely dry, while the ranges and south-east are relatively wet. Overall, South Australia is the driest Australian state.
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South Korea has moderate annual rainfall.
Southeast Asia is experiencing increased rainfall due to several factors, including climate change, which intensifies weather patterns and creates more extreme precipitation events. Additionally, changes in land use and deforestation can alter local climates and contribute to increased rainfall. The region's tropical climate, characterized by monsoons, also plays a significant role, with variations in monsoon patterns leading to heavier rainfall in certain areas. These combined factors are contributing to the observed increase in rainfall across the region.
The district with lowest rainfall in kerala is thiruvananthapuram in southern kerala it received only 523 mm rainfall in the south west monsoon .mainly southern kerala recieves the lowest rainfall. thiruvanthapuram recorded 27 % deficient rainfall during the south west monsoon rainfall in kerala.
Monsoons occur primarily in South and Southeast Asia, as well as parts of Africa and Australia. These seasonal wind patterns bring heavy rainfall to these regions during the summer months.
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