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Monsoon continental climate
From Wikipedia, the free encyclopedia
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]
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![Thumb image](http://upload.wikimedia.org/wikipedia/commons/thumb/4/43/Dw_climate.png/640px-Dw_climate.png)