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The intensity and structure of Typhoon Nanmadol (2011) was affected by the land mass when it passed between Luzon and Taiwan.Furthermore, Nanmadol was also embedded within the environment with high vertical wind shear during that period, which induced clearly asymmetric convection around the storm.The Weather Research and Forecasting model with finest resolution of 3.3 km was applied to perform numerical experiments to understand the effects of terrain and environmental vertical wind shear on the intensity, structure and asymmetric convection of Nanmadol when it passed these two islands.The terrain-removed sensitivity experiments were also conducted to elucidate the relative role of terrain in the forming of the asymmetric convection of the storm.