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Impact of ENSO-Like Tropical Pacific Decadal Variability on the Relative Frequency of El Nino and La Nina Events

机译:Enso-like热带太平洋额外变异对El Nino和La Nina事件的相对频率的影响

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摘要

Observational and modeling studies show that the relative frequency of El Nino and La Nina varies in association with El Nino-Southern Oscillation (ENSO)-like tropical Pacific decadal variability (TPDV), but the causality of the linkage remains unclear. This study presents evidence that ENSO-like TPDV affects the frequency of ENSO events, particularly of El Nino, through a set of climate model experiments. During the positive phase of TPDV, tropical Pacific warming relative to the Indian and Atlantic Oceans increases the occurrence of anomalous westerly winds over the western equatorial Pacific in late boreal winter-spring, triggering more El Nino and fewer La Nina events. The opposite happens for the negative TPDV phase. The La Nina frequency is also influenced by oceanic adjustments following El Nino, which tends to counteract the effect of wind changes. The mean state control of ENSO offers a potential opportunity for decadal predictions of climate extremes.
机译:观察和建模研究表明,El Nino和La Nina的相对频率与El Nino-Southern振荡(ENSO)相结合的热带太平洋二等变异性(TPDV),但连锁的因果关系尚不清楚。 本研究提出了证据,即通过一组气候模型实验,enso-limity TPDV影响ENSO事件,特别是EL NINO的频率。 在TPDV的阳性阶段,热带太平洋相对于印度和大西洋的热化增加了西部赤道太平洋在北部北方冬季春天的异常西风的发生,触发了更多的El Nino和La Nina活动。 对于负TPDV阶段,相反。 LA NINA频率也受EL NINO之后的海洋调整的影响,这往往会抵消风变化的影响。 ENSO的平均国家控制为气候极端的近代预测提供了潜在的机会。

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