Climate Rewires Long-Distance Connections ✛ ✎

Original: "Climate change alters teleconnections"
· Eran Vos, Peter Huybers, Eli Tziperman
arXiv:2512.22678 · 2025-12-27 · arXiv non-exclusive · independent analysis · 2 min
Greenhouse gases have already altered the invisible threads linking weather across the planet.

A warm ocean off the coast of Peru can make winter in Moscow unusually mild. Such invisible threads linking weather in distant corners of the planet are called teleconnections. They were once thought of as permanent wiring: the signal sources may pulse, but the wires themselves lie still. New work shows that greenhouse gases have already rewired this circuitry.

Scientists compared two thirty-year periods: 1960–1990 and 1990–2020. They took temperature maps for every point on the globe and looked at how strongly these maps correlate with five major climate modes, including El Niño, the Indian Ocean Dipole, and the Pacific Decadal Oscillation. It turned out that over thirty years, connections changed over a fifth of the planet's surface. For El Niño, significant shifts affected 20% of grid cells; for the Indian Ocean Dipole, 15%; and for global mean temperature, 28%.

What changes is not the signal sources themselves but the medium through which the signal travels. The amplitude of El Niño has barely changed, yet its influence on remote regions has been reconfigured.

To distinguish an anthropogenic shift from natural variability, scientists compared the observed change in connections with a thousand random changes derived from a control model run without human influence. The observed shift was larger than any of the thousand random ones. This means the probability of attributing it to natural fluctuations is less than one in a thousand. Before this work, it was unclear whether the teleconnections themselves change under greenhouse gas forcing or whether the observed shifts were random. Now it is clear: the global restructuring of teleconnections between 1960–1990 and 1990–2020 cannot be explained by natural variability. It is attributed to human influence.

The sign change of the ENSO teleconnection in northeastern Africa means that El Niño, which used to bring warmth there, may now bring cooling.

S_{obs} = \frac{\langle \Delta C_{obs}, \Delta C_{model}^{forced} \rangle_F}{\|\Delta C_{model}^{forced}\|_F^2}
A number showing how similar the observed shift is to the model response to anthropogenic forcing; S>0 means similarity in sign, S=1 means identity.
Concepts
El Niño ENSO North Atlantic Oscillation Teleconnection La Niña interannual variability El Niño-Southern Oscillation natural variability seasonal cycle spring predictability barrier seasonal forcing Multivariate ENSO Index TAO/TRITON moorings ERSST relative ONI NOAA CPC climate network North Equatorial Countercurrent Jin-Timmermann model ocean-atmosphere coupling