The land areas are divided into South East Asia (Vietnam, Philippines, South China), Middle East Asia (East China, including the Island of Taiwan), and North East Asia (Korean Peninsula and Japan). Time series of the annual number of landfalling TCs in each area are formed, both for all TCs having tropical storm intensity and for those reaching typhoon (TY) intensity at landfall.
The results show that none of the time series possesses any statistically significant trend, which suggests that global warming does not lead to more landfalls in any of the regions in Asia. Each time series show large interannual (2-8 years), interdecadal (8-16 years) and even multi-decadal (16-32 years) variations. In some periods, this number varies in unison among all regions of Asia. In others, one region might have above-normal number of landfalling TCs while the other regions have below-normal numbers. In general, at multi-decadal time scales, the number of TC or TY landfall in each region is well correlated with that of the total number of TCs or TYs over the western North Pacific. Some of the variations can be explained by similar variations in the Pacific Decadal Oscillation, El Nino or the Arctic Oscillation.
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