El Niño as Conductor: How Climate Ties Together Earth's Rotation and Carbon Dioxide ✎

Original: "Quantifying the Multivariate ENSO Index (MEI) coupling to CO2 concentration and to the length of day variations"
arXiv:1206.5828 · 2012-06-25 · arXiv non-exclusive · independent analysis · 2 min
Extreme values of the El Niño index are synchronously linked to changes in CO₂ concentration and day length.

A vast tongue of warm water rises to the surface of the tropical Pacific, and the entire climate system begins to resonate in unison. This is El Niño, the most powerful natural climate oscillation, affecting weather from Australia to Alaska. Scientists have long noticed that during strong El Niño events, something happens to atmospheric carbon dioxide and to Earth's rotation itself. But the connection remained as fuzzy as an echo in a large hall.

New work turns that echo into a clear rhythm. The researchers took three observational records spanning decades: the MEI index, which combines six meteorological parameters over the tropical Pacific; CO₂ concentrations at the Mauna Loa station in Hawaii; and day length (LOD), which varies slightly above and below the familiar 24 hours. After removing seasonal cycles, they compared how these quantities change from year to year. It turns out that El Niño peaks precede peaks in the CO₂ growth rate by three months, and troughs in the rate of change of day length by four months.

The connection turned out to be so simple that it can be expressed with two numbers. Each unit of the MEI index corresponds to an increase in the CO₂ accumulation rate of 0.55 parts per million per year and a slowdown in the rate of change of day length of 0.27 milliseconds per year.

This is not just a statistical quirk. The coefficients show how a single mechanism governs different spheres of the planet. El Niño's warm waters cause the ocean and land to release more carbon dioxide, while the redistribution of mass changes Earth's moment of inertia, speeding up its rotation. The conductor raises the baton, and both the woodwinds and the percussion come in precisely on cue.

But even orchestras have off nights. In 1991, the eruption of Mount Pinatubo in the Philippines spewed so much ash and aerosol into the atmosphere that ecosystem respiration slowed, and diffuse light altered photosynthesis. The link between El Niño and CO₂ was disrupted for two years. This exception only underscores the rule: when there are no external disturbances, the rhythm holds.

Today, these coefficients could serve as a tuning fork for climate models. If a model reproduces the lags and the numbers, it correctly captures the coupling between ocean, atmosphere, and Earth's rotation. In this way, empirical correlations become a verification tool. And although the mechanism that generates El Niño itself remains a mystery, we now know how it conducts the entire planet.

The eruption of Mount Pinatubo in 1991 so strongly affected the global carbon cycle that it disrupted the link between El Niño and the CO₂ growth rate for two years.

\Delta CO_2/год = 0.55 \times MEI
Conversion coefficient between the El Niño index and the CO₂ growth rate
\Delta LOD/год = -0.27 \times MEI
Conversion coefficient between the El Niño index and the rate of change of day length
Concepts
Multivariate ENSO Index ENSO El Niño index El Niño-Southern Oscillation TAO/TRITON moorings Southern Oscillation spring predictability barrier Jin-Timmermann model La Niña NOAA CPC relative ONI ERSST natural variability recharge oscillator model North Equatorial Countercurrent interannual variability ocean-atmosphere coupling Warm water volume Teleconnection monsoon