近百年东亚登陆台风的长期振动

ISSN 1004-4965

CN 44-1326/P

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近百年东亚登陆台风的长期振动

汪铎, 陆叔鸣, 陈继芳, 张镡

文章导航 > 热带气象学报 > 1986 > (4): 343-348

汪铎, 陆叔鸣, 陈继芳, 张镡. 近百年东亚登陆台风的长期振动[J]. 热带气象学报, 1986, (4): 343-348.

引用本文:

汪铎, 陆叔鸣, 陈继芳, 张镡. 近百年东亚登陆台风的长期振动[J]. 热带气象学报, 1986, (4): 343-348.

Wang Duo, Lu Shuming, Chen Jifang, Zhang Tan. LONG-TERM FLUCTUATION OF THE LANDING TYPHOON OVER THE EAST ASIA DURING LAST 100 YEARS[J]. Journal of Tropical Meteorology, 1986, (4): 343-348.

Citation:

Wang Duo, Lu Shuming, Chen Jifang, Zhang Tan. LONG-TERM FLUCTUATION OF THE LANDING TYPHOON OVER THE EAST ASIA DURING LAST 100 YEARS[J]. Journal of Tropical Meteorology, 1986, (4): 343-348.

汪铎, 陆叔鸣, 陈继芳, 张镡. 近百年东亚登陆台风的长期振动[J]. 热带气象学报, 1986, (4): 343-348.

引用本文:

汪铎, 陆叔鸣, 陈继芳, 张镡. 近百年东亚登陆台风的长期振动[J]. 热带气象学报, 1986, (4): 343-348.

Wang Duo, Lu Shuming, Chen Jifang, Zhang Tan. LONG-TERM FLUCTUATION OF THE LANDING TYPHOON OVER THE EAST ASIA DURING LAST 100 YEARS[J]. Journal of Tropical Meteorology, 1986, (4): 343-348.

Citation:

Wang Duo, Lu Shuming, Chen Jifang, Zhang Tan. LONG-TERM FLUCTUATION OF THE LANDING TYPHOON OVER THE EAST ASIA DURING LAST 100 YEARS[J]. Journal of Tropical Meteorology, 1986, (4): 343-348.

近百年东亚登陆台风的长期振动

1.
浙江师范学院
2.
江西省气象台
3.
温州市气象台
4.
北京大学

计量
- 文章访问数: 997
- HTML全文浏览量: 2
- PDF下载量: 686
- 被引次数: 0
出版历程
- 收稿日期: 1985-10-03
- 修回日期: 1986-04-15

LONG-TERM FLUCTUATION OF THE LANDING TYPHOON OVER THE EAST ASIA DURING LAST 100 YEARS

1.
Zhejiang Normal University
2.
Jiangxi Meteorological Service
3.
Wenzhou Meteorological Service
4.
Beijing Univrsity

摘要: 按不同地段统计分析了1884—1980年期间东亚登陆台风个数以偏多期与偏少期交替为特征的长期振动。发现东亚沿太平洋的多数地段上登陆台风数的长周期振动的主要周期为20年左右,较短周期的振动主要有5～6年和2～3年周期。不同地段上长期振动的差异主要表现在周期、位相和振幅上。还发现登陆台风数的长期振动与春夏季节关键地区的大型气压环流的低频振动有某种关联。

Abstract: In this paper, the long-term fluctuations of the landing typhoon which are characterised as the inversion of more/less periods are statistically analyzed in terms of various coastal regions in the East Asia during 1884-1980.The fluctuation periods of most coastal regions are about 20-yr (low frequency)and 5-6-yr(high frequency). The differences among the long-term fluctuations over various coastal regions are shown with period, phase and swing.Some relationship between the long-term fluctuations of the landing typhoon and low frequency fluctuations of large-scale pressure circulation are illustrated finally.

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文章访问数: 997
HTML全文浏览量: 2
PDF下载量: 686
被引次数: 0

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