Abstract

The El Niño-Southern Oscillation (ENSO) has been shown to manifest as primarily two types, the eastern Pacific (EP) type and central Pacific (CP) type, in terms of the zonal positions of the sea surface temperature (SST) anomalies. This study focuses on examining the predictability of the two types of ENSO by developing statistical models for their corresponding Niño indices, which have their own distinct key precursors. The results show that the statistical predictability of the Niño indices representing the two types of ENSO primarily originates from the preceding variations in the equatorial Pacific upper-ocean heat content and the surface zonal wind stress, which intrinsically reflect the zonally uniform and contrasted thermocline patterns, respectively. The traditional Niño3 and Niño4 indices are more predictive than the Niño indices of the EP and CP ENSO types; however, all the indices are subject to predictability barriers with different timings and intensities, which might be weakened by introducing additional external precursors. The EP ENSO indices have overall higher skills than the CP indices, in which the statistical model has much higher skill scores than persistence forecast for the EP ones while it does less for the CP ones. We demonstrate that the precursors outside the tropical Pacific, e.g., the Indian Ocean Dipole, North Pacific oscillation, North American dipole, and Southern Hemispheric SST modes, except the northern tropical Atlantic SST, as suggested in previous studies, only make limited contributions to improving the prediction skills of the two ENSO types at specific initial months and leads compared to a benchmark model built using the equatorial Pacific heat content and zonal wind stress indices. This is primarily because these precursors have already transferred most of their signals into the variation of the two indices in the benchmark model. We further show that conditionally adding the northern tropical Atlantic SST precursor to the benchmark could provide considerable additional prediction skill scores for both types of ENSO and weaken the intensity of the ENSO predictability barriers that occur during boreal spring‒summer.

Highlights

  • The El Niño-Southern Oscillation (ENSO) dominates interannual climate variability in the tropics and has a remarkable impact on the global climate (e.g., Rasmusson and Carpenter 1982; Brönnimann 2007; Zhang et al 2017)

  • The analysis has demonstrated that the northern tropical Atlantic (NTA) sea surface temperature (SST) during the middle winter‒early spring can significantly improve the predictions of the WP (EP) ENSO indices in the following months, while the other precursors from outside the tropical Pacific that are focused on in this study have limited contributions to improving the prediction skills of both types of ENSO relative to the benchmark model built with the equatorial Pacific warm water volume (WWV) and zonal wind stress (ZWS) precursors

  • We examined the predictability of the two types of ENSO by building up statistical models that include both the equatorial Pacific WWV and ZWS precursors as a benchmark version and attempted to involve several external precursors from outside the tropical Pacific to further improve the statistical models

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Summary

Introduction

The El Niño-Southern Oscillation (ENSO) dominates interannual climate variability in the tropics and has a remarkable impact on the global climate (e.g., Rasmusson and Carpenter 1982; Brönnimann 2007; Zhang et al 2017). Studies of the statistical predictability of the two ENSO types are necessary, in addition to those based on dynamical models, because many studies have revealed the physical mechanisms for motivation and maintenance of the two ENSO types Both the equatorial Pacific thermocline and the zonal wind variations play important roles in motivating and maintaining the two ENSO types (Ashok et al 2007; Ren and Jin 2013), and the recharge oscillator mechanism proposed by Jin (1997a, b) occurs in both ENSO types (Ren and Jin 2013), suggesting that both the WWV and ZWS precursors are expected to be applicable to statistical predictions of the two types of Niño indices.

Data and methods
Relationships of the Niño indices with the heat content and zonal wind stress
Benchmark models and prediction skills for different Niño indices
Contributions to the prediction skills of Niño indices
Dependence on the equatorial Pacific WWV and ZWS indices
Establishment and evaluations of models for the two ENSO types
Summary and discussions
Full Text
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