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  1. Jan 9, 2016 · Unlike equatorial wet climate, monsoon climate is characterized by distinct wet and dry seasons associated with seasonal reversal of winds. Floods in wet season and droughts in dry season are common. Usually there are three seasons namely summer, winter and rainy season. Occur within 5° to 30° N and S of the equator.

  2. In parts of India monsoon rainfall has decreased since 1950. Meanwhile, in the Philippines and other areas of the western North Pacific, the amount of monsoon rain has increased. Weak monsoon rains produced drought and famine over large parts of Africa in the 1970s and 1980s, but the West African monsoon rains have recovered somewhat since then.

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  4. The North American Monsoon PDF version : Until the late 1970s, there was serious debate about whether a monsoon truly existed in North America. However, considerable research, which culminated in the Southwest Arizona Monsoon Project (SWAMP) in 1990 and 1993, established the fact that a bonafide monsoon, characterized by large-scale wind and rainfall shifts in the summer, develops over much of Mexico and the intermountain region of the U.S. Published papers at the time called this pattern by ...

  5. Jun 7, 2016 · The significant southwest monsoon rainfall is a by-product of air passing over large areas of warm equatorial ocean, stimulating increased levels of evaporation from the ocean’s surface; the southwest monsoon air, now laden with water vapour, cools as it moves north and as it rises over land; at some point the air is no longer able retain its moisture and precipitates copious volumes to irrigate rice fields and drench rainforests, sometimes causing severe flooding.

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  7. Aug 22, 2022 · What is the North American monsoon? A monsoon is a seasonal change in wind patterns that delivers rainfall to a large area or continent, typically causing dry winters and wet summers. Although ...

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