| 近58年来登陆中国热带气旋气候变化特征 |
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| 引用本文： | 杨玉华,应明,陈葆德.近58年来登陆中国热带气旋气候变化特征[J].气象学报,2009,67(5):689-696. |
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| 作者姓名： | 杨玉华 应明 陈葆德 |
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| 作者单位： | 中国气象局上海台风研究所,上海,200030;中国气象局台风预报技术重点开放实验室,上海,200030 |
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| 基金项目： | 中国气象局气候变化专项，国家自然科学基金资助项目 |
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| 摘 要： | 利用1949-2006年<台风年鉴>和<热带气旋年鉴>资料,主要分析了1949-2006年登陆中国热带气旋的频数、登陆位置、登陆季节延续期和登陆强度等要素及其概率分布的年际和年代际变化特征.结果表明:近58年来,登陆中国热带气旋年频数有减少趋势,但登陆时达台风强度的年频数变化不明显;按登陆地点分区统计发现,登陆华南地区的热带低压及(强)热带风暴年频数以减少为主,而登陆东部地区的热带气旋年频数变化不明显.登陆点历年最北位置(最南位置)有南移(弱的北移)趋势,导致登陆点历年南北最大纬度差逐渐减小,这表明热带气旋登陆区域更为集中,在23°-35°N增多,而在35°N以北和23°N以南以减少为主.登陆中国热带气旋季节延续期缩短了近1个月.热带气旋年平均登陆强度及其概率分布偏度有增加趋势,表明登陆的强台风有增加;登陆中国华南和东部地区的台风强度都有增强趋势,前者比后者趋势更明显.另外,热带气旋年最大登陆强度差长期呈现减小的趋势.
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| 关 键 词： | 登陆热带气旋 登陆位置 陆强度 偏度 |
| 收稿时间： | 2009/1/31 0:00:00 |
| 修稿时间： | 4/6/2009 12:00:00 AM |
The climatic changes of landfall tropic al cyclones in China over the past 58 years |
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| YANG Yuhu,YING Ming and CHEN Baode.The climatic changes of landfall tropic al cyclones in China over the past 58 years[J].Acta Meteorologica Sinica,2009,67(5):689-696. |
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| Authors: | YANG Yuhu YING Ming and CHEN Baode |
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| Institution: | Shanghai Typhoon Institute of the China Meteorological Administration, Shang hai 200030, China; Laboratory of Typhoon Forecast Technique/CMA, Shanghai 200030, China,Shanghai Typhoon Institute of the China Meteorological Administration, Shang hai 200030, China; Laboratory of Typhoon Forecast Technique/CMA, Shanghai 200030, China and Shanghai Typhoon Institute of the China Meteorological Administration, Shang hai 200030, China; Laboratory of Typhoon Forecast Technique/CMA, Shanghai 200030, China |
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| Abstract: | By using the data from the Tropical Cyclone Yearbooks, changes of landfall tropical cyclones (TCs) in China over the past 58 years (1949 - 2006) were analyzed, in terms of their tracks, numbers, duration, intensity, probability distributions as well as in-terannual and decadal variabilities. The results indicate that the landfall TCs numbers have decreased but the numbers hardly changed for typhoons. The frequency decreased evidently for tropical depressions and (strong) tropical storms landed in southern China, but the variation of frequency of TCs over eastern China is not obvious. Over the past 58 years, the most northern latitude of landfall TCs for each year tends to be more southward, and the most southern latitude turns to be more northward, resulting in a decrease of the south-north range of landfall TCs, i.e., more TCs tend to make landfall between 23°N and 35°N, and fewer in the north of 35°N and south of 23°N. The landfall season is decreased by about one month. The intensity of landfall TCs has increased, and the intensi-ty difference between the strongest and the weakeat TCs reduced. Furthermore, the skew of intensity shows an upward tendency, in-dicating the proportion of stronger landfall TCs has increased. Finally, the annual averaged intensity of landfall TCs has enhanced for both southern China and eastern China, with a stronger increase appearing in the former than the latter. |
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| Keywords: | Landfall TC Landfall location Landfall intensity Skew |
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