Why El Niño Arrives in Winter: The Ocean as a Pendulum with Memory ✎

Original: "A delay differential model of ENSO variability, Part 2: Phase locking, multiple solutions, and dynamics of extrema"
· Ilya Zaliapin, Michael Ghil
arXiv:1003.0028 · 2010-02-26 · arXiv non-exclusive · independent analysis · 1 min
The ocean remembers wind pushes for months, and this memory makes warm and cold events recur at the same time of year.

A swing does not start rocking right after a push; it responds with a delay. The ocean is the same: the wind blows today, but the surface temperature changes several months later. According to the authors, it is this memory of the ocean that makes El Niño and La Niña arrive at the same time of year.

The model replaces the entire ocean with a single number: temperature. Its rate of change depends on what the temperature was earlier, not what it is now. Seasonal winds add a rhythm, like a person pushing a swing. The researchers tried different delay lengths and push strengths and found that warm events almost always occur in winter. Cold events, however, occur in summer, even though in nature they also happen in winter.

Under the same conditions, the model can behave in different ways: sometimes it produces dozens of different rhythms, and all of them are stable. Slightly change the initial temperature, and the ocean jumps to another regime.

This means that a simple scheme is not enough to explain La Niña. Another mechanism is needed to shift the cold phase to winter. But the main finding is different: even such a simple system with memory can be very capricious and abruptly change its behavior. That is why predicting El Niño and La Niña is hard, and it will become even harder as the climate warms.

The name 'El Niño' (Spanish for 'the boy child') comes from the warm current off the coast of Peru often appearing around Christmas, in honor of the baby Jesus.

Concepts
ENSO El Niño-Southern Oscillation Jin-Timmermann model spring predictability barrier La Niña recharge oscillator model El Niño index Multivariate ENSO Index TAO/TRITON moorings Pacific decadal oscillation Warm water volume ERSST equatorial wave propagation natural variability seasonal forcing seasonal cycle mixed mode oscillations relative ONI Bjerknes feedback ocean-atmosphere coupling