Storm surge along the China's Zhe-Min coast is addressed using the tightly coupled surge model of ADCIRC+SWAN. In this study, we primarily focus on the effects of surge-tide interaction and wave set-up/set-down. And the influences of intensity and landing moment of tropical cyclone (TC) are also presented. The results show that: water elevation without considering tide-surge interaction tends to be underestimated/overestimated when TC lands during astronomical low/high tide; tide-surge coupling effect is more pronounced north of TC track (more than 0.7 m in our cases); irrelevant to TC's intensity, wave set-up south of TC track is negligible because the depth-related wave breaking doesn't occur in water body blown towards open seas.