谢义炳, 陈受钧, 张一良, 黄寅亮. 1963: 东南亚基本气流与台风发生的一些事实的統計与分析. 气象学报, (2): 206-217. DOI: 10.11676/qxxb1963.020
引用本文: 谢义炳, 陈受钧, 张一良, 黄寅亮. 1963: 东南亚基本气流与台风发生的一些事实的統計与分析. 气象学报, (2): 206-217. DOI: 10.11676/qxxb1963.020
HSIEH YI-PING, CHEN SHOU-JUN, CHANG I-LIANG, HUANG YIN-LIANG. 1963: A PRELIMINARILY STATISTIC AND SYNOPTIC STUDY ABOUT THE BASIC CURRENTS OVER SOUTHEASTERN ASIA AND THE INITIATION OF TYPHOONS. Acta Meteorologica Sinica, (2): 206-217. DOI: 10.11676/qxxb1963.020
Citation: HSIEH YI-PING, CHEN SHOU-JUN, CHANG I-LIANG, HUANG YIN-LIANG. 1963: A PRELIMINARILY STATISTIC AND SYNOPTIC STUDY ABOUT THE BASIC CURRENTS OVER SOUTHEASTERN ASIA AND THE INITIATION OF TYPHOONS. Acta Meteorologica Sinica, (2): 206-217. DOI: 10.11676/qxxb1963.020

东南亚基本气流与台风发生的一些事实的統計与分析

A PRELIMINARILY STATISTIC AND SYNOPTIC STUDY ABOUT THE BASIC CURRENTS OVER SOUTHEASTERN ASIA AND THE INITIATION OF TYPHOONS

  • 摘要: 本文根据近年来的资料,对东南亚低緯度基本气流与台风发生的关系进行了統計与个例分析.結果指出,北半球夏季西太平洋极大多数台风发生在赤道西风与北半球信风間交界面的东端.赤道西风尺度大,比較稳定,可視作夏季低緯度基本气流,而台风可視为这种基本气流与另一基本气流——信风——間交界面上的涡旋.台风发生的时間、地点及次数与低緯度基本气流的位置及强度有密切的关系。低緯度基本气流的位置与强度具有一个月以上的长周期式振动,因而可供台风发生频率的中期預报参考.

     

    Abstract: The relation between the basic currents of the low latitudes and the initiation of typhoons is investigated statistically and synoptically by means of recent aerological data. It is shown that about 80外of typhoons developed in the eastern part of the equatorical convergence zone between the equatorial westeries and trade wind of West Pacific Ocean. The equatorial westeries is a large scale and quasi-steady phenomeanon therefore it is probably reasonable to be called "basic current" and typhoons are considered as vortices of smaller scale. There is a quite definite relationship between the time, position, frequency of the initiation of typhoons and the position, strength of the basic currents in the low latitudes. There is a quasi-periodical variation of the strength.and position of the basic currents with a period longer than one month. This fact may be helpful for the extended forecast the initiation and development of typhoons.

     

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