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Tropical monsoon are most commonly found in Africa (West and Central Africa), Asia (South and Southeast Asia), South America and Central America. This climate also occurs in sections of the Caribbean, North America, and northern Australia.
The tropical monsoon climate experiences abundant rainfall like that of the tropical rain forest climate, but it is concentrated in the high-sun season. Being located near the equator, the tropical monsoon climate experiences warm temperatures throughout the year.
tropical monsoon and trade-wind littoral climate, major climate type of the Köppen classification characterized by small annual temperature ranges, high temperatures, and plentiful precipitation (often more than wet equatorial, or Af, climates in annual total).
An area of tropical monsoon climate (occasionally known as a sub-equatorial, tropical wet climate or a tropical monsoon and trade-wind littoral climate) is a tropical climate subtype that corresponds to the Köppen climate classification category Am.
A tropical monsoon climate is characterized by high temperatures and significant seasonal rainfall, typically found in regions near the equator. This climate features a pronounced wet season during which heavy rains occur, followed by a dry season.
The tropical monsoon climate experiences abundant rainfall like that of the tropical rain forest climate, but it is concentrated in the high-sun season. Being located near the equator, the tropical …
There are three main seasons of tropical monsoon climate: the cool dry season is from fall to late winter, the hot dry season is in the spring and the rainy or monsoon season is near or during the summer months.
A monsoon is a seasonal change in the direction of the prevailing, or strongest, winds of a region. Monsoons cause wet and dry seasons throughout much of the tropics. Monsoons are most often associated with the Indian Ocean. Monsoons always blow from cold to warm regions.
Tropical monsoon and trade-wind littoral climate, major climate type of the Köppen classification characterized by small annual temperature ranges, high temperatures, and plentiful precipitation (often more than wet equatorial, or Af, climates in annual total).
Photograph. Climate is the long-term pattern of weather in a particular area. Weather can change from hour-to-hour, day-to-day, month-to-month or even year-to-year. A region’s weather patterns, usually tracked for at least 30 years, are considered its climate. Photograph by Walter Meayers Edwards, National Geographic. Leveled by.