On the Surface Independent Signals Within the ENSO Events

Mingqiang Fang
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Abstract

By analyzing the two types of El Nino Southern-Oscillation (ENSO) indices, i.e., the Central Pacific (CP) type index and the Eastern Pacific (EP) type index by Ren and Jin (2011), this study finds that the low correlation between the two types of indices by some previous studies should be reconsidered. Then based on previous ideas of the unified Nino index systems, the new ocean surface regions for the CP and EP El Nino indices’ calculation are defined. The features of the new CP and EP El Nino indices are consistent with sea surface temperature anomaly (SSTA) evolution along the Pacific equator. This study suggests that, concerning the El Nino characteristics, the CP and EP El Nino indices are not necessarily independent of each other; but their differences are almost absolutely independent of the unified Nino region SSTA. The results quantitatively confirm the relationship between the Trans-Nino Index (TNI) and Nino 3.4 indices (which are nearly independent of each other and provide different flavors for each El Nino event). Results presented here contribute to a better understanding of the nature of the El Nino events.
论ENSO事件中的地表独立信号
本研究通过对Ren and Jin(2011)的两类厄尔尼诺南方涛动(ENSO)指数,即中太平洋(CP)型指数和东太平洋(EP)型指数的分析,发现需要重新考虑以往一些研究中两类指数之间的低相关性。然后在前人统一的厄尔尼诺指数体系思想的基础上,定义了CP和EP厄尔尼诺指数计算的新海表区域。新CP和EP厄尔尼诺指数的特征与太平洋赤道海温异常(SSTA)演变一致。研究表明,就厄尔尼诺特征而言,CP和EP厄尔尼诺指数并不一定是相互独立的;但它们的差异几乎完全独立于统一的尼诺区海温。结果定量地证实了反尼诺指数(TNI)和尼诺3.4指数之间的关系(它们几乎相互独立,为每个厄尔尼诺事件提供了不同的味道)。本文提出的结果有助于更好地理解厄尔尼诺事件的性质。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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