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Official Journal of the Asia Oceania Geosciences Society (AOGS)

Fig. 10 | Geoscience Letters

Fig. 10

From: Extreme precipitation trends in Northeast China based on a non-stationary generalized extreme value model

Fig. 10

Spatial 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 level

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