• Source: Monsoon continental climate

The Monsoon continental climate, also known as Manchurian climate, is a continental climate sub-type. It is a monsoon climate with large thermal range. It is located mainly in East Asia, Korea and Manchuria. Its dry season happens during the winter ("Dw" meaning "Dry Winter").




Sub-types


Hot summer Manchurian climate, classified as a Hot summer continental climate (Dwa) under the Köppen classification: Mean temperature is above to 0 °C, but under to 10 °C. Precipitations about of 500 mm. This climate is located in Northeast China and Korean Peninsula. (Examples: Beijing, Harbin, Shenyang, Pyongyang, Seoul, North Platte)
Warm summer or hemiboreal Manchurian climate, classified as a Warm summer continental or hemiboreal climate (Dwb) under the Köppen classification: Northeast of China, far Southeastern Siberia and North Dakota. (Examples: Heihe, Yanji, Vladivostok, Khabarovsk, Irkutsk, Calgary)
Monsoon subpolar, classified as a Subarctic or boreal climate (Dwc) under the Köppen classification: Zones of China, northern Mongolia and southern Siberia. Also in parts of Canada and Alaska. (Examples: Mohe, Yushu City, Tsetserleg, Delta Junction)
Monsoon subpolar with severe winters, classified as a Subarctic or boreal climate with severe winters (Dwd) under the Köppen classification: Extreme climate in small zones of Siberia. (Examples: Allakh-Yun, Delyankir)




See also


Continental climate
Humid continental climate
Continental mediterranean climate
Köppen climate classification




References

Kata Kunci Pencarian:

• Hujan
• Geografi Thailand
• Periode Afrika basah
• Monsoon continental climate
• Humid continental climate
• Continental climate
• Temperate climate
• Subarctic climate
• Oceanic climate
• Köppen climate classification
• Humid subtropical climate
• Climate of Seoul
• Climate of Vietnam