The present winter climate of continental China is associated with cold air activity.The cold air forming Siberian high pressure comes from the Northern Barents Sea.Northwestern Kara Sea and Northern Atlantic Ocean (f...The present winter climate of continental China is associated with cold air activity.The cold air forming Siberian high pressure comes from the Northern Barents Sea.Northwestern Kara Sea and Northern Atlantic Ocean (fig.1). in other words, mainly fromthe cold northern sea surface. west and east to Novaya Zemlya and the sea surface south展开更多
Research on long-term climatic variation on the Chinese Loess Plateau has demonstrated that loess is mainly the dust deposits transported by the northern wind of the winter monsoon, and that the paleosol accreted by r...Research on long-term climatic variation on the Chinese Loess Plateau has demonstrated that loess is mainly the dust deposits transported by the northern wind of the winter monsoon, and that the paleosol accreted by rather slow dust accumulation was closely related to a strengthened summer monsoon. The climate over the Chinese展开更多
基金Project supported by the National Natural Science Foundation of China.
文摘The present winter climate of continental China is associated with cold air activity.The cold air forming Siberian high pressure comes from the Northern Barents Sea.Northwestern Kara Sea and Northern Atlantic Ocean (fig.1). in other words, mainly fromthe cold northern sea surface. west and east to Novaya Zemlya and the sea surface south
文摘Research on long-term climatic variation on the Chinese Loess Plateau has demonstrated that loess is mainly the dust deposits transported by the northern wind of the winter monsoon, and that the paleosol accreted by rather slow dust accumulation was closely related to a strengthened summer monsoon. The climate over the Chinese
