Researchers at University of Tsukuba and the Meteorological Research Institute have identified how atmosphere–ocean interactions in the midlatitudes reinforce the East Asian winter monsoon (EAWM). During strong monsoon seasons, cold air outbreaks from the Eurasian continent cool the midlatitude western North Pacific (WNP). This oceanic cooling, in turn, alters atmospheric circulation in a manner that further intensifies the monsoon.
Midlatitude atmosphere-ocean feedback reinforces the east Asian winter monsoon
