Although there may be shared characteristics, the divergence between PPT found in Tropical Monsoon Climates (e.g. India) and Cool Temperate Western Maritime Climates (such as the United Kingdom) can have substantial implications. "Monsoon" derives from Arabic and pertains to a "season", where wind movements have a significant impact on this climate by causing considerable shifts in direction throughout various seasons. Additionally, within this particular climate, there is an evident wet season that transpires during summer.
The western coast of this area is mostly affected by heavy precipitation, which occurs during its three seasons: March to May, June to September, and October to February. During the months of March through May, high temperatures and drought are typical.
Between June and September, the majority of the yearly rainfall occurs in frequent heavy rainfalls, which account for approximately 80% of the tota
...l precipitation. During this time, there is a drop in temperature. From October to February, the rainy season concludes and typically results in clear skies and mild temperatures.
A Cool Temperate Western Maritime climate can be found in the United Kingdom and is positioned at 40` - 60` North and South of the equator. This climate experiences slightly more rain during the winter compared to summer, with light intensity rainfall. The climate is known to be changeable with no marked seasonal differences, and is characterized by common clouds and precipitation.
Extreme temperatures are present, with both very hot and very cold weather conditions. These climates share seasonal and regional variations. The tropical monsoon climate has extremely hot or wet seasons, with increased rainfall during the summer. The Cool Temperate Western Maritime climate has less distinct seasons, but experiences moderately increased precipitatio
and colder temperatures during winter.
Both mountainous regions in Cool Temperate Western Maritime Climates and Tropical Monsoon Climates experience heavier rainfall. However, the two climate types differ in terms of rainfall intensity and total annual precipitation. In Cool Temperate Western Maritime Climates, precipitation is typically lighter and shorter, whereas in Tropical Monsoon Climates, rainfall is heavy and alternates with periods of drought. As a result, the total annual precipitation in India's Tropical Monsoon Climate is approximately 11,000 mm, while the UK's Cool Temperate Western Maritime Climate only receives around 1,300 mm.
Although having some resemblances, the two climates differ significantly which sets them apart from each other.
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