Fig. 4: Sensitivity of the extreme precipitation to anthropogenic warming and the thermodynamic and dynamic components. | npj Climate and Atmospheric Science

Fig. 4: Sensitivity of the extreme precipitation to anthropogenic warming and the thermodynamic and dynamic components.

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

Fig. 4

Averaged 72-h extreme precipitation sensitivity (orange bars; units: % K−1) and its associated dynamic (blue bars; units: % K−1) and thermodynamic (green bars; units: % K−1) components in relation to changes in surface temperature due to anthropogenic warming (units: K) for the average of a the two sub-regions, b the northern sub-region, and c the southern sub-region.

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