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作 者:LIAODechun ZHOUYonghong LIAOXinhao
机构地区:[1]ShanghaiAstronomicalObservatory,ChineseAcademyofSciences,Shanghai200030,China [2]NationalAstronomicalObservatories,ChineseAcademyofSciences,Beijing100012,China [3]UnitedCenterforAstro-GeodynamicsResearch,ChineseAcademyofSciences,Shanghai200030,China
出 处:《Chinese Science Bulletin》2003年第16期1709-1713,共5页
基 金:supported by the National Natural Science Foundation of China(NNSFC)(Grant Nos.10273018,10133010,19833030 and 19973011);Science and Technology Development Fund of Shanghai(Grant No.JC14012).
摘 要:Using the length-of-day (LOD) data series de-rived from astronomical observations made by various mod-ern space techniques, southern oscillation index (SOI) and anomalies of sea surface temperature (SST) in tropical Pa-cific Ocean, the inter-annual components of these data series are obtained by the technique of band filtering from January 1962 to October 2002. It is found that a new ENSO event has already occurred in 2002 and been detected by the inter- annual LOD. It is shown by the wavelet analysis that the component with a period of about 46 years and the quasi-biennial component are out of phase during 2001 2002, which consequently suggests that the new ENSO event cannot be a strong one.Using the length-of-day (LOD) data series de-rived from astronomical observations made by various mod-ern space techniques, southern oscillation index (SOI) and anomalies of sea surface temperature (SST) in tropical Pa-cific Ocean, the inter-annual components of these data series are obtained by the technique of band filtering from January 1962 to October 2002. It is found that a new ENSO event has already occurred in 2002 and been detected by the inter- annual LOD. It is shown by the wavelet analysis that the component with a period of about 46 years and the quasi-biennial component are out of phase during 2001 2002, which consequently suggests that the new ENSO event cannot be a strong one.
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