Abstract

The real-time prediction skill for El Niño-Southern Oscillation has not improved steadily during the twenty-first century. One important reason is the season-dependent predictability barrier (PB), and another is due to the diversity of El Niño. In this paper, an approach to data analysis for predictability is developed to investigate the season-dependent PB phenomena of two types of El Niño events by using the monthly mean data of the preindustrial control (“pi-Control”) runs from several coupled model outputs in CMIP5 experiments. The results find that predictions for Central Pacific El Niño (CP-El Niño) suffered from summer PB, whereas those for Eastern Pacific El Niño (EP-El Niño) are mainly interfered with by spring PB. The initial errors most frequently causing PB for CP- and EP-El Niño are revealed and they emphasize that the initial sea temperature accuracy in the Victoria mode (VM) region in the North Pacific is more important for better predictions of the intensity of the CP-El Niño, whereas that in the subsurface layer of the west equatorial Pacific and the surface layer of the southeast Pacific is of more concern for better predictions of the structure of CP-El Niño. However, for EP-El Niño, the former is indicated to modulate the structure of the event, whereas the latter is shown to be more effective in predictions of the intensity of the event. Obviously, for predicting which type of El Niño will occur, more attention should be paid to the initial sea temperature accuracy in not only the subsurface layer of the west equatorial Pacific and the surface layer of the southeast Pacific but also the region covered by the VM-like mode in the North Pacific. This result provided guidance aiming at how to initialize model in predictions of El Niño types.

Highlights

  • The El Niño-Southern Oscillation (ENSO) phenomenon represents the strongest interannual climate fluctuation on earth, alternating between warm (El Niño) and cold (La Niña) conditions, which influences weather and climate on aGreat progress has been made in understanding ENSO dynamics and physics in recent decades (Neelin 1991; Jin 2000; Levine and Jin 2010; Wang 2018)

  • This indicates that these two composite initial errors can cause summer predictability barrier (PB) for CP-El Niño events in all six models, and if they are filtered from corresponding initial analysis from control forecasts, a significant improvement in forecast skill can be found in the CP-El Niño predictions made by the six models

  • We have revealed the initial errors that often cause summer PB for CP El Niño and spring PB for EP El Niño and explain why they always behave similar to a La Niña-like evolving mode and the corresponding physical mechanism

Read more

Summary

Introduction

The El Niño-Southern Oscillation (ENSO) phenomenon represents the strongest interannual climate fluctuation on earth, alternating between warm (El Niño) and cold (La Niña) conditions, which influences weather and climate on a. Tian and Duan (2015) traced the evolution of a conditional nonlinear optimal perturbation (CNOP) that acts as the initial error with the largest negative effect on the El Niño predictions by using the Zebiak–Cane model (Zebiak and Cane 1987) They found that for both types of El Niño, their initial errors that have the largest effect on prediction uncertainties are mainly concentrated in the central and eastern tropical Pacific. In addition to the previously mentioned questions, based on multimodel outputs, we attempt to identify the initial errors that frequently result in season-dependent PB for the two types of El Niño events. We use model data to explore the above questions; we further expect to obtain initial errors that result in season-dependent PB The former is involved with discrete data, whereas the latter is associated with dynamical behavior of error growth.

Data and an approach to data analysis for ENSO predictability
Persistence barrier of El Niño
The summer PB for CP El Niño and its related initial error growth
The spring PB for EP El Niño and its related initial error growth
Implications for ENSO predictions
Findings
Summary and discussion
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call