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The Köppen climate classification is the most widely used climate classification system. [2] It defines a tropical climate as a region where the mean temperature of the coldest month is greater than or equal to 18 °C (64 °F) and does not fit into the criteria for B-group climates, classifying them as an A-group (tropical climate group). [3]
The ecosystems of the tropical marine climate have to adapt to the dry season. Plants during the dry season must conserve water/moisture. However, the extent of the adaptation depends much on the annual rainfall.
Relationship of Earth's axial tilt (ε) to the tropical and polar circles: the Tropic of Cancer is a subsolar point only at the June solstice, and the Tropic of Capricorn is only at the December solstice [7]
The mid-level African easterly jet stream north of the equator is considered to play a crucial role in the West African monsoon, [10] and helps form the tropical waves which march across the tropical Atlantic and the eastern part of the Pacific during the warm season. [11]
Worldwide zones of tropical monsoon climate (Am). 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.
Hardiness zones in China. The northern extremities of both Heilongjiang and Inner Mongolia have a subarctic climate [5] with long, severe winters, and short, warm summers. [6] In contrast, most of Hainan Island and parts of the extreme southern fringes of Yunnan have a tropical climate. [5]
In 2003, a controversial paper written by Willie Soon and Sallie Baliunas was published in the journal after being accepted by editor Chris de Freitas. [2] [3] The article reviewed 240 previous papers and concluded that "Across the world, many records reveal that the 20th century is probably not the warmest or a uniquely extreme climatic period of the last millennium". [3]
Köppen climate classification of Myanmar, 1980 to 2016.. The climate of Myanmar varies depending on location and in the highlands, on elevation. The climate is subtropical/tropical and has three seasons, a "cool winter from November to February, a hot summer season in March and April and a rainy season from May to October, dominated by the southwest monsoon."