The Mongolian Plateau (MP) is located in the eastern part of arid Central Asia (ACA). Climatically, much of the MP is dominated by the westerly circulation and has an arid and semi-arid climate; however, the eastern part of the MP is also influenced by the East Asian summer monsoon (EASM) and has a humid and semi-humid climate. Recently, several studies have shown that precipitation variability in the MP differs from that in western ACA but is consistent with that in the EASM region.
Click here for original story, The spatial consistency of summer rainfall variability between the Mongolian Plateau and North China
Source: Phys.org