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Hao Chunjiang,Zhang Lin,Xue Zhenhe,Xie Simei.Antarctic sea ice and ENSO event[J].Acta Oceanologica Sinica,1993,(4):549-561
Antarctic sea ice and ENSO event
Antarctic sea ice and ENSO event
投稿时间:1993-02-06  修订日期:1993-03-16
DOI:
中文关键词:  
英文关键词:
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作者单位
Hao Chunjiang National Research Center for Marine Environment Forecasts, State Oceanic Administration, Beijing 100081, China 
Zhang Lin National Research Center for Marine Environment Forecasts, State Oceanic Administration, Beijing 100081, China 
Xue Zhenhe National Research Center for Marine Environment Forecasts, State Oceanic Administration, Beijing 100081, China 
Xie Simei National Research Center for Marine Environment Forecasts, State Oceanic Administration, Beijing 100081, China 
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中文摘要:
      The characteristic low-frequency oscillation of the sea surface temperature anomaly (SSTA) of ENSO related regions, Niño 1+2, Niño 3, Niño 4 and Niño West, and the Southern Oscillation index (SOI) is analyzed with the method of maximum entropy spectrum.Antarctic sea ice is divided into 4 regions, i.e.East Antarctic is Region Ⅰ (0°-120°E), the region dominated by Ross Sea ice is Region Ⅱ (120°E-120°W), the region dominated by Ross Sea ice is Region Ⅲ (120°W-0°), and the whole Antarctic sea ice area is Region Ⅳ.Also, the month-to-month correlation series of the sea ice with ENSO from contemporary to 5-years lag is calculated.The optimum correlation period is selected from the series.The characteristics and the rules obtained are as follows.1.There are a common 4-years main period of the SSTA of Niños 1+2, 3 and 4, a rather strong 4-years secondary period and a quasi-8-years main period of that of Niño West.
英文摘要:
      The characteristic low-frequency oscillation of the sea surface temperature anomaly (SSTA) of ENSO related regions, Niño 1+2, Niño 3, Niño 4 and Niño West, and the Southern Oscillation index (SOI) is analyzed with the method of maximum entropy spectrum.Antarctic sea ice is divided into 4 regions, i.e.East Antarctic is Region Ⅰ (0°-120°E), the region dominated by Ross Sea ice is Region Ⅱ (120°E-120°W), the region dominated by Ross Sea ice is Region Ⅲ (120°W-0°), and the whole Antarctic sea ice area is Region Ⅳ.Also, the month-to-month correlation series of the sea ice with ENSO from contemporary to 5-years lag is calculated.The optimum correlation period is selected from the series.The characteristics and the rules obtained are as follows.1.There are a common 4-years main period of the SSTA of Niños 1+2, 3 and 4, a rather strong 4-years secondary period and a quasi-8-years main period of that of Niño West.
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