Why Warm Ocean Waves Heat the Planet More Than We Thought ✎

Original: "Comment on "Influence of the Southern Oscillation on tropospheric temperature" by J. D. McLean, C. R. de Freitas, and R. M. Carter"
arXiv:0908.1828 · 2009-08-13 · arXiv non-exclusive · independent analysis · 2 min
El Niño leaves behind heat that accumulates for decades and explains half of the warming since 1960.

A bathtub of warm water sits under an open tap, but the drain isn't closed. Each El Niño wave adds a bit of heat, and only part of it flows out. Over time, the water in the tub gets hotter, even if the greenhouse gas tap has barely been touched.

Scientists have long struggled to understand why Earth is warming so quickly. They knew that El Niño is a natural warming of the Pacific Ocean that occurs every few years. But all previous attempts to link it to global warming failed because researchers looked only at individual years, not at the cumulative total. The new study did something simple: they took all Southern Oscillation Index values since 1960 and added them up, like collecting raindrops in a barrel.

The largest accumulated heat sum from El Niño occurred in 1976, when the air was cold, and the smallest occurred in the record-warm year 1998.

It turned out that this accumulated sum explains half of the temperature changes in the upper air and 54% at the surface. A simple model with only accumulated El Niño works almost as well as a model with only greenhouse gases. This doesn't mean emissions aren't warming the planet, but perhaps their contribution has been overestimated.

The bathtub from the first sentence hints at the answer: the ocean doesn't just slosh back and forth; it remembers heat. Warm water from El Niño partially sinks to depth and returns the following year, like tea that's been topped up with boiling water before being finished. If so, climate models that ignore this ocean memory will make wrong predictions.

The cumulative SOI index peaked at 948 in 1976, coinciding with one of the coldest periods in the troposphere over the past 50 years, while the minimum of -172 in 1998 coincided with the record warmest year.

cSOI(t) = \sum_{i=1}^{t} SOI_i
Sum of all previous Southern Oscillation Index values up to time t
T = 0.29 - 0.00055 \cdot cSOI - 0.0061 \cdot SOI - 1.8 \cdot V - 0.0011 \cdot SSN
Model linking temperature to cumulative SOI, SOI itself, volcanic aerosols, and solar activity
T = -0.15 - 0.00025 \cdot cSOI - 0.0051 \cdot SOI - 1.6 \cdot V - 0.0007 \cdot SSN + 0.19 \cdot AF
Model adding anthropogenic forcing to the equation
Concepts
ENSO Southern Oscillation El Niño-Southern Oscillation Multivariate ENSO Index El Niño index Jin-Timmermann model spring predictability barrier TAO/TRITON moorings La Niña recharge oscillator model ERSST relative ONI NOAA CPC natural variability Teleconnection seasonal forcing UAH satellite record Indian Ocean Dipole seasonal cycle monsoon