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30—50天低频振荡和准双周振荡对持续异常的影响
引用本文:孙永罡,陈久康.30—50天低频振荡和准双周振荡对持续异常的影响[J].南京气象学院学报,1992,15(3):368-376.
作者姓名:孙永罡  陈久康
作者单位:黑龙江省气象台 (孙永罡),南京气象学院(陈久康)
基金项目:75-09-01经费资助
摘    要:

关 键 词:持续异常  低频振荡  准双周振荡

THE INFLUENCE OF 30-50 DAY LOW-FREQUENCY FLUCTUATION AND QUASI-14 DAY FLUCTUATION ON THE PERSISTENT ANOMALIES
Sun Yonggang,Chen Jiukang Meteorological Observatory of Heilongjiang Province Nanjing Institute of Meteorology.THE INFLUENCE OF 30-50 DAY LOW-FREQUENCY FLUCTUATION AND QUASI-14 DAY FLUCTUATION ON THE PERSISTENT ANOMALIES[J].Journal of Nanjing Institute of Meteorology,1992,15(3):368-376.
Authors:Sun Yonggang  Chen Jiukang Meteorological Observatory of Heilongjiang Province Nanjing Institute of Meteorology
Institution:Sun Yonggang;Chen Jiukang Meteorological Observatory of Heilongjiang Province Nanjing Institute of Meteorology
Abstract:Using the data of the 500 hPa pentad anomaly of 14 winters (1971-1984) inthe Northern Hemisphere,the geographical distribution of the general circulation anoma-lies in the Northern winter is analysed. The effects of the 30-50 day low-frequencyfluctuation and quasi-14 day fluctuation on the persistent anomalies in their evolutionare studied. Results show that the time scale of the persistent anomalies is mainly associ-ated with the 30-50 day low-freqency fluctuation. It is found that Alaska is the keyregion of not only the persistent anomalies but also the 30-50 day low-frequency fluc-tuation. The persistent circulation anomalies and weather-climate anomalies are chieflydominated by the 30-50 day low-frequency fluctuation.
Keywords:persistent anomaly  30--50 day low--frequency fluctuation  quasi--14 day fluctuation
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