Based on the analysis of 30 storm surge processes (1952-1974) along the Fujian and Guangdong coastal area, it can be seen that there are differences among the typhoon surges owing to the various tracks of typhoon. The landfalling typhoon is the main track bringing about disasters. The typhoon, moving parallel to the coast or in the distance，generally may not produce heavy surge. A typhoon surge by no means rises or falls steadily in the entire process, some associated oscillations with various periods superimpose on the surge and drastically develops with the forced wave. An entire process of a typhoon surge may last 3-5 days, the larger the scale of typhoon and the lower its speed, the 1onger the duration of the surge. As concerns the landfalling typhoon, the occurrence time of peak surge of each station which lies on the right side of the moving direction of typhoon lags from the north to the south, like a wave traveling from the north to the south. According to the preliminary analysis, the main wave of the typhoon surge in the Strait has some character1stics of tidal wave, however, a serial inertiogravitational waves may be generated out off the Strait, particularlly under the topographic effect of the East China Sea, the typhoon morving northward along the coastline may lead to the generation of the ''edge wave”. Due to the interaction between surge and astronomical tide, the surge curves shows an evident tidal oscillation. Here, the relationship between the speed of typhoon and surges as well as the correlation diagram between the occurrence time of peak surge and speed of typhoon and distance are given. Finally, the effect of the meteorological factors of single station on the typhoon surges are discussed, the empirical forecasting equations are presented. In addition, the feasible range and practical results of the equations are analyzed.