Fig. 3: Evolutionary characteristics of the remnant of Typhoon Doksuri. | npj Climate and Atmospheric Science

Fig. 3: Evolutionary characteristics of the remnant of Typhoon Doksuri.

From: Locally opposite responses of the 2023 Beijing–Tianjin–Hebei extreme rainfall event to global anthropogenic warming

Fig. 3

a Track of the remnant of Typhoon Doksuri as simulated in the CTL (black lines) and NAT (red lines) experiments, with the overlay representing the daily average horizontal wind vectors at 850 hPa for the CTL experiment on 30 July 2023. The thick lines denote the tracks from the ensemble mean, whereas the thin lines represent those of the ensemble members. b The intensity (hPa) of the remnant of Typhoon Doksuri for the CTL (black lines) and NAT (red lines) simulations, where the thick and thin lines represent the intensities derived from the ensemble mean and the ensemble members, respectively. The time–latitude Hovmöller diagrams of the average maximum radar reflectivity (units: dBZ) over the region 110.0–122.0°E for the c CTL and d NAT simulations. The dashed black reference lines along 36.8°N and 40.0°N are representative locations in the southern and northern sub-regions, respectively, shown in Fig. 2d.

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