Climate as a Road Map: Bifurcations and Resonances of El Niño ✎

Original: "Bifurcation analysis of delay-induced resonances of the El-Nino Southern Oscillation"
· Bernd Krauskopf, Jan Sieber
arXiv:1109.2818 · 2011-09-13 · arXiv non-exclusive · independent analysis · 2 min
Scientists have mapped all the roads along which the Pacific climate wanders.

The Pacific Ocean does not breathe evenly but in bursts. Every few years, its warm waters stir, and then Australia suffocates from drought while Peru is flooded with rain. This phenomenon is called El Niño, and it resembles a traveler wandering along an invisible road map.

Kelvin waves, which carry warm anomalies across the Pacific, travel at about 2–3 meters per second, covering 10,000 kilometers in roughly two months.

This map is not drawn on paper. It is hidden in the equations that describe how the ocean and atmosphere exchange heat. The main feature of these equations is delay. A warm patch in the ocean does not immediately change the wind, and the wind does not immediately change the currents. Time passes, and the response returns to the system like an echo in the mountains. According to scientists, it is precisely these delays that set the rhythm of El Niño.

Previously, to understand this rhythm, scientists ran computer models and watched how they behaved. This is like a traveler simply walking along roads without having a map. He might find one or two trails, but he would not see the whole network of crossroads and dead ends. The new work proposes a different approach: to build the map itself. To do this, the authors applied a method that mathematicians call bifurcation analysis. It allows not just observing the system's behavior, but finding all possible regimes of its operation and the boundaries between them.

At the parameter point used in the original work by Cziperman, the system lies just to the left of the 1:3 resonance tongue, which explains the observed non-periodic dynamics close to a three-year cycle.

The result is a detailed map showing regions where the climate oscillates strictly periodically and regions where it behaves chaotically. For example, if the average coupling strength between ocean and atmosphere is small, the system is calm. But once a certain boundary is crossed, stable rhythms with periods of three or four years emerge. These rhythms are called resonant because they synchronize with the annual cycle, like a pendulum swinging in time with pushes.

The road map for climate is not just a beautiful abstraction. It shows how sensitive El Niño is to changes in parameters that scientists know only approximately. If the real climate is near a boundary between different regimes, even a small measurement error can lead to an incorrect forecast. Now, with the map in hand, researchers can better understand where our traveler is wandering and where he might turn in the future.

Kelvin waves that carry warm anomalies across the Pacific Ocean travel at about 2–3 meters per second, crossing 10,000 kilometers in roughly two months.

In Kim Stanley Robinson's novel 'Forty Signs of Rain', climate models with feedbacks and delays play a key role in predicting abrupt weather changes, echoing the idea of ENSO's sensitivity to parameters.

\frac{d}{dt}h(t) = bG[\kappa(t-\tau_1)h(t-\tau_1)] - cG[\kappa(t-\tau_2)h(t-\tau_2)] - dh(t)
The rate of change of the thermocline anomaly equals the difference between a positive feedback with delay τ1 and a negative feedback with delay τ2, minus dissipation
G(x) = \begin{cases} b_+ \tanh(x/b_+) & \text{если } x \ge 0 \\ b_- \tanh(x/b_-) & \text{если } x < 0 \end{cases}
Nonlinear function that limits the growth of anomalies and introduces asymmetry between warm and cold phases
\kappa(t) = k_0 + d_k \sin(\omega t)
Mean value k0 plus a sinusoidal variation with amplitude dk and frequency ω, corresponding to 12 months
Concepts
El Niño-Southern Oscillation ENSO Jin-Timmermann model El Niño index recharge oscillator model Multivariate ENSO Index Southern Oscillation spring predictability barrier La Niña TAO/TRITON moorings equatorial wave propagation ERSST Bjerknes feedback delayed oscillator theory natural variability NOAA PMEL / TAO seasonal forcing mixed mode oscillations Teleconnection seasonal cycle