《Table 1.Experimental design in this study.》

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《Potential impacts of enhanced tropical cyclone activity on the El Nio–Southern Oscillation and East Asian monsoon in the mid-Piacenzian warm period》

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*Including the Pacific and North Atlantic（10°35°N；110°E20°W）and South Indian Ocean and southwestern Pacific（10°35°S；50°E150°W）.Vertical diffusivity is not changed over the North Indian Ocean，as TC intensity and power dissipation were lower

PI and MP are integrated for 1550 years and 3850 years to reach quasi-equilibrium，with the energy imbalance at the top of the atmosphere being～0.1 and-0.01 W m-2，respectively.Initialized from MP，the two sensitivity experiments are then run for 500 years.We analyze the last 50 years of model outputs in each experiment.A summary of the experimental design is given in Table 1.