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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]
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The Köppen climate classification system was modified further within the Trewartha climate classification system in 1966 (revised in 1980). The Trewartha system sought to create a more refined middle latitude climate zone, which was one of the criticisms of the Köppen system (the climate group C was too general). [10]: 200–1
The following is a list of terrestrial ecoregions of the People's Republic of China and the Republic of China, according to the World Wide Fund for Nature.. The transition between two of the planet's eight terrestrial biogeographic realms – the Palearctic, which includes temperate and boreal Eurasia, and Indomalaya, which includes tropical South and Southeast Asia – extends through ...
Köppen climate types of China. Owing to tremendous differences in latitude, longitude, and altitude, the climate of China is extremely diverse, ranging from tropical in the far south to subarctic in the far north and alpine in the higher elevations of the Tibetan Plateau.
Köppen-Geiger climate classification map for mainland China [130] China's climate is mainly dominated by dry seasons and wet monsoons, which lead to pronounced temperature differences between winter and summer. In the winter, northern winds coming from high-latitude areas are cold and dry; in summer, southern winds from coastal areas at lower ...
China lies in two of the world's major ecozones, the Palearctic and the Indomalaya. In the Palearctic zone mammals such as the horse, camel, and jerboa are found. Among the species found in the Indomalaya region are the leopard cat, bamboo rat, treeshrew, and various other species of monkeys and apes. Some overlap exists between the two regions ...
Today, the most commonly used climate map is the Köppen climate classification, developed by Russian climatologist of German descent and amateur botanist Wladimir Köppen (1846–1940), which divides the world into five major climate regions, based on average annual precipitation, average monthly precipitation, and average monthly temperature.