Fig. 10From: Extreme precipitation trends in Northeast China based on a non-stationary generalized extreme value modelSpatial distribution of the MK trend analysis method for a, b 500 hPa height field; c, d 850 hPa specific humidity field and wind field in early summer (ES) and mid-summer (MS). The direction of the arrow indicates the wind direction, and the length of the arrow indicates the wind force. Dotting means the correlation coefficients at the 0.05 significance levelBack to article page