Landfalling characteristics of the tropical cyclones generated in the South China Sea

Tracks of tropical cyclones (TCs) in the South China Sea (SCS) during 1970-2010 can mainly be divided into two categories: Westward (including west and northwest) and Eastward (east and northeast). TCs moving westward tend to make landfall along the South china or Vietnam coast, while those moving eastward tend to dissipate in the ocean or make landfall on Taiwan, Philippine Islands or occasionally the South China coast. During spring (April-May), there are 17 TCs generated in the SCS, among which 13 moves eastward, but only 4 moves westward. A total of 95 TCs forms in the SCS during TC peak season (June-September), among which 71 TCs move westward, about three times more than that moving eastward (24). During October-December, 33 TCs move westward and 12 eastward. The variability of TC track direction is investigated on intraseasonal, seasonal and inter-annual scale circulation. It is found that TC landfall activities are related to Madden-Julian Oscillation (MJO), El Nino-Southern Oscillation (ENSO), monsoon activities and TC genesis locations.