Fig. 6: Difference in WPSH anomalies between the four WRF downscaled CMIP5/6 future period (2080-2100, red contours) and the historical period (1979–2003, black) during the July-October season. | npj Climate and Atmospheric Science

Fig. 6: Difference in WPSH anomalies between the four WRF downscaled CMIP5/6 future period (2080-2100, red contours) and the historical period (1979–2003, black) during the July-October season.

From: Environmental controls on future projections of western North Pacific tropical cyclone maximum intensity

Fig. 6

(a) RCP45, (b) RCP85, (c) SSP245, and (d) SSP585. Here, the WPSH anomalies are defined to be the deviation of the mean 500–hPa geopotential height relative to the domain average. Superimposed is the corresponding horizontal wind difference between each future scenario and the historical period at the same 500 hPa level.

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