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Data from the China Meteorological Administration and ERA-Interim are used to examine the environmental characteristics of landfalling tropical cyclones (TCs) with abrupt intensity change.The results show that,of all 657 landfalling TCs during 1979-2017,71%,70% and 65% of all landfalling TDs,TSs and TYs,respectively,intensify.Of all the 16595 samples,4.0% and 0.2% of typhoons and tropical storms,respectively,experience over-water rapid intensification (RI) process during their life cycle.Meanwhile,4.5% and 0.6% of typhoons and tropial storms,respectively,undergo overwater rapid decay (RD).These two kinds of cases,i.e.,RI and RD,are used to analyze their associated large-scale conditions.Comparisons show that the RI cases are generally on the south side of the strong west Pacific subtropical high (WPSH);warm sea surface temperatures (SSTs) and sufficient water vapor fluxes existing in RI samples is a dominant feature that is conducive to the development of TCs.Also,the moderate low-level relative vorticity is favorable for TC intensification.On the contrary,the RD TCs are located on the west side of the WPSH;significant decreasing SSTs and low-level water vapor transport may synergistically contribute to RD.Simultaneously,low-level relative vorticity seems to be unfavorable for the development of TCs.