Abstract

Large uncertainties exist in real-time predictions of the 2015 El Niño event, which have systematic intensity biases that are strongly model-dependent. It is critically important to characterize those model biases so they can be reduced appropriately. In this study, the conditional nonlinear optimal perturbation (CNOP)-based approach was applied to an intermediate coupled model (ICM) equipped with a four-dimensional variational data assimilation technique. The CNOP-based approach was used to quantify prediction errors that can be attributed to initial conditions (ICs) and model parameters (MPs). Two key MPs were considered in the ICM: one represents the intensity of the thermocline effect, and the other represents the relative coupling intensity between the ocean and atmosphere. Two experiments were performed to illustrate the effects of error corrections, one with a standard simulation and another with an optimized simulation in which errors in the ICs and MPs derived from the CNOP-based approach were optimally corrected. The results indicate that simulations of the 2015 El Niño event can be effectively improved by using CNOP-derived error correcting. In particular, the El Niño intensity in late 2015 was adequately captured when simulations were started from early 2015. Quantitatively, the Niño3.4 SST index simulated in Dec. 2015 increased to 2.8 °C in the optimized simulation, compared with only 1.5 °C in the standard simulation. The feasibility and effectiveness of using the CNOP-based technique to improve ENSO simulations are demonstrated in the context of the 2015 El Niño event. The limitations and further applications are also discussed.

Highlights

  • The El Niño and Southern Oscillation (ENSO) phenomenon has been recognized as the most predictable short-term climate anomaly in the climate system (Philander 1983; Wang and Picaut 2004)

  • A striking feature associated with that event was the slow evolution of a warm sea surface temperature (SST) anomaly in the western tropical Pacific through 2014 and early 2015: a steady SST warming in the equatorial Pacific in 2014, a dip in February 2015, and a rapid warming in May that persisted through the summer and fall of 2015

  • Its onset occurred in early 2015, a rapid amplification of the warm SST anomalies occurred in late spring and summer, and a mature stage was reached in late 2015 (Zhang and Gao 2017)

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Summary

Introduction

The El Niño and Southern Oscillation (ENSO) phenomenon has been recognized as the most predictable short-term climate anomaly in the climate system (Philander 1983; Wang and Picaut 2004). Various coupled models have been developed and used to make 6-month and longer real-time ENSO predictions in advance and with reasonable success. Coupled models with different degrees of complexity still have systematic biases with large uncertainties in the real-time prediction of ENSO (Jin et al 2008; Luo et al 2008; Zhang and Gao 2016b); for a summary of the model ENSO forecasts, see the International Research Institute for Climate and Society (IRI) website at http://iri.columbia.edu/climate/ENSO/currentinfo/update. ENSO predictions are widely spread across models, with each model having characteristic biases. Understanding error sources for ENSO predictions is critically important for finding a way by which biases can be reduced appropriately (Blumenthal 1991; Goswami and Shukla 1991). Errors in initial conditions (ICs) and model parameters (MPs) are two main sources that limit ENSO

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