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").^{[1][failed verification]}

• 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^{[disambiguation needed]}, 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)

• Continental climate
• Humid continental climate
• Continental mediterranean climate
• Köppen climate classification

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