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STATISTICAL CHARACTERISTICS ON TROPICAL CYCLONESLANDFALL IN CHINA

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  • With the data from the Tropical Cyclone Yearbooks between 1970 and 2001, statistical analyses were performed to study the climatic features of landfall TCs (noted as TCs hereafter) in China with particular attention focused on landfall frequency, locations, sustaining, decaying, transition, intensification and dissipation etc. The results indicate that the sustaining periods of TC over land are quite different for different landfall spots, and increased from Guangxi to Zhejiang. The most obvious decreasing of TC intensity occurs mainly within 12 hours after landfall. The stronger a TC is,the more it decays. The areas over which TCs are dissipated can be in Heilongjiang, the northernmost, and Yunnan, the westernmost. Besides, Guangxi is an area with high dissipating rate and subject to TC dissipation as compared with the other coastal regions.
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LI Ying, CHEN Lian-shou, ZHANG Sheng-jun, et al. STATISTICAL CHARACTERISTICS ON TROPICAL CYCLONESLANDFALL IN CHINA [J]. Journal of Tropical Meteorology, 2006, 12(2): 150-158.
LI Ying, CHEN Lian-shou, ZHANG Sheng-jun, et al. STATISTICAL CHARACTERISTICS ON TROPICAL CYCLONESLANDFALL IN CHINA [J]. Journal of Tropical Meteorology, 2006, 12(2): 150-158.
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STATISTICAL CHARACTERISTICS ON TROPICAL CYCLONESLANDFALL IN CHINA

Abstract: With the data from the Tropical Cyclone Yearbooks between 1970 and 2001, statistical analyses were performed to study the climatic features of landfall TCs (noted as TCs hereafter) in China with particular attention focused on landfall frequency, locations, sustaining, decaying, transition, intensification and dissipation etc. The results indicate that the sustaining periods of TC over land are quite different for different landfall spots, and increased from Guangxi to Zhejiang. The most obvious decreasing of TC intensity occurs mainly within 12 hours after landfall. The stronger a TC is,the more it decays. The areas over which TCs are dissipated can be in Heilongjiang, the northernmost, and Yunnan, the westernmost. Besides, Guangxi is an area with high dissipating rate and subject to TC dissipation as compared with the other coastal regions.

LI Ying, CHEN Lian-shou, ZHANG Sheng-jun, et al. STATISTICAL CHARACTERISTICS ON TROPICAL CYCLONESLANDFALL IN CHINA [J]. Journal of Tropical Meteorology, 2006, 12(2): 150-158.
Citation: LI Ying, CHEN Lian-shou, ZHANG Sheng-jun, et al. STATISTICAL CHARACTERISTICS ON TROPICAL CYCLONESLANDFALL IN CHINA [J]. Journal of Tropical Meteorology, 2006, 12(2): 150-158.
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