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Reduction of the East Asian winter monsoon interannual variability after the mid-1980s and possible cause
2012
Chinese Science Bulletin
The East Asian winter monsoon (EAWM) consists of subsystems such as the Siberian high, Aleutian low, East Asian trough, low-level northerly wind and high-level East Asian jet stream. It is revealed that the interannual variation of the EAWM-related atmospheric circulation has exhibited an obvious weakening since the mid-1980s. During 1956-1980, significant negative correlations between the EAWM and sea surface temperature are observed in the oceans along the east coast of East Asia, accompanied
doi:10.1007/s11434-012-5468-5
fatcat:txoxh6g5sne2bfn6yhyfpahqka