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The Monsoon continental climate, also known as Manchurian climate (Dw), is a continental climate sub-type. It is bassically a monsoon climate with large termic range. It is mainly located in East Asia, Korea and Manchuria. Its dry season happens in winter.[1]
Sub-types
- Hot summer manchurian climate (Dwa): Mean temperature is above to 0 °C, but under to 10 °C. Precipitations about of 500 mm. This climate is located in China, North Korea and South Korea.
- Warm summer or hemiboreal manchurian climate (Dwb): Northeast of China and North Dakota.
- Monsoon subpolar (Dwc): Zones of China, North of Mongolia and South Siberia. Also in someplace of Canadá and Alaska.
- Monsoon hipercontinental (Dwd): Extrem climate in small zones of Siberia.
See also
- Continental climate
- Humid continental climate
- Mediterranean continental climate
- Köppen climate classification
References
- ^ Bernhard Paul Weninger 2014, Neolithisation of the Aegean and Southeast Europe during the 6600–6000 calBC period of Rapid Climate Change. Modern Position of the Intertropical Convergence Zone (ITCZ) in July and January. Researchgate DOI: 10.4312/dp.41.1 University of Cologne