摘要
55-year (1949 - 2003) data sets are used to study the statistical characteristics in intensity change of the tropical cyclones (TC) over the western North Pacific. According to the mathematical meaning of average value and standard deviation, the abruptly intensifying, gradually intensifying, stable intensity, gradually weakening and abruptly weakening of TC intensity are defined and the statistical characteristics, such as inter-decadal variation, inter-annual variation, inter-monthly variation, and regional distribution, etc. are analyzed. Main results are as follows: (1) From 1949 to 2003, there were 1886 TCs, averaging at 34.29 TCs per year. After 1995, the number of TCs dropped dramatically with less than 30 per year. 3.56% of the total were abruptly intensifying samples, and 3.31% were weakening samples. (2) For the annual mean, all but the stable group tend to decrease with the shift of decades as far as the overall change of the 6-h isallobaric process is concerned. (3) The abruptly intensifying TC seldom occurs over mid- and high-latitude area (north of 30°N) and low-latitude area and sometimes occurs around the islands and continent. Basically there is no gradually intensifying of TC over mid- and high- latitude area (north of 30°N and west of 125°E), in offshore Chinese waters. The gradually weakening and abruptly weakening TCs usually occur offshore China, west of 125 °E, but seldom over low-latitude area (0 - 5°N).
55-year （ 1949 - 2003） data sets are used to study the statistical characteristics in intensity change of the tropical cyclones （TC） over the western North Pacific. According to the mathematical meaning of average value and standard deviation, the abruptly intensifying, gradually intensifying, stable intensity, gradually weakening and abruptly weakening of TC intensity are defined and the statistical characteristics, such as inter-decadal variation, inter-annual variation, inter-monthly variation, and regional distribution, etc. are analyzed. Main results are as follows： （1） From 1949 to 2003, there were 1886 TCs, averaging at 34.29 TCs per year. After 1995, the number of TCs dropped dramatically with less than 30 per year. 3.56% of the total were abruptly intensifying samples, and 3.31% were weakening samples. （2） For the annual mean, all but the stable group tend to decrease with the shift of decades as far as the overall change of the 6-h isallobaric process is concerned. （3） The abruptly intensifying TC seldom occurs over mid- and high-latitude area （north of 30°N） and low-latitude area and sometimes occurs around the islands and continent. Basically there is no gradually intensifying of TC over mid- and high- latitude area （north of 30°N and west of 125°E）, in offshore Chinese waters. The gradually weakening and abruptly weakening TCs usually occur offshore China, west of 125°E, but seldom over low-latitude area （0 - 5°N）.
基金
Natural Science Foundation of China (4057575018, 40205008)
Special project on climatechange from the China Meteorological Administration (CCSF2007-13)
