Climate Prediction Department, APEC Climate Center, Busan, South Korea.
Department of Atmospheric Sciences, University of Hawaii at Manoa, Honolulu, HI, USA.
Sci Rep. 2017 Jul 20;7(1):6029. doi: 10.1038/s41598-017-05221-3.
This study uses retrospective forecasts made using an APEC Climate Center seasonal forecast model to investigate the cause of errors in predicting the amplitude of El Niño Southern Oscillation (ENSO)-driven sea surface temperature variability. When utilizing Bjerknes coupled stability (BJ) index analysis, enhanced errors in ENSO amplitude with forecast lead times are found to be well represented by those in the growth rate estimated by the BJ index. ENSO amplitude forecast errors are most strongly associated with the errors in both the thermocline slope response and surface wind response to forcing over the tropical Pacific, leading to errors in thermocline feedback. This study concludes that upper ocean temperature bias in the equatorial Pacific, which becomes more intense with increasing lead times, is a possible cause of forecast errors in the thermocline feedback and thus in ENSO amplitude.
本研究使用 APEC 气候中心季节性预测模型进行的回溯预测,调查了预测厄尔尼诺-南方涛动(ENSO)驱动的海面温度变化幅度的误差的原因。当利用 Bjerknes 耦合稳定性(BJ)指数分析时,发现随着预测提前期的增加,ENSO 幅度的增强误差很好地由 BJ 指数估计的增长率误差表示。ENSO 幅度的预测误差与热带太平洋上强迫的温跃层斜率响应和海面风响应的误差密切相关,导致温跃层反馈的误差。本研究得出的结论是,赤道太平洋上层海洋温度的偏差,随着提前期的增加而加剧,这可能是温跃层反馈和 ENSO 幅度预测误差的原因。