October Arctic Oscillation
“A negative AO in October sets up a cold winter.”
- Correlation, Nov–Mar
- −0.05
- Dec–Feb
- −0.02
- vs 10-yr normal
- −6%
Every October the same signs come out: Siberian snow, the QBO, the Blob, a cold October. We scored ten of them against the winter's gas-weighted heating degree days, 1951–2026, and again as real forecasts made only from earlier winters.
“A negative AO in October sets up a cold winter.”
“If the Atlantic blocks in October, it blocks all winter.”
“Fast October snow over Siberia means a cold eastern US.”
“It's how fast the snow spreads, not how much there is.”
“Warm water off the West Coast builds the ridge that sends cold east.”
“Easterly QBO, cold winter.”
“Same idea, lower in the stratosphere.”
“The vortex has a memory.”
“This winter will be like last winter.”
“As goes October, so goes the winter.”
Across all winters the link is modest (r = −0.28), and it is not linear. Weak El Niños are as scattered as neutral winters, while the five strongest since 1950 were all mild. In strong El Niño winters, a forecast built on trend plus El Niño strength cut the error against the 10-year normal by about 100 heating degree days, in 98% of bootstrap resamples. Six winters is a small sample, and the 2026/27 El Niño is forecast to be stronger than any of them. The ENSO forecast itself is on /nino/.
Target: US heating degree days (65 °F base) from ERA5, weighted by each state's residential and commercial natural gas use (EIA, 2021–25 mean), November–March and December–February, as a departure from the 1951–2026 linear trend. These weights reproduce an industry desk's monthly gas-weighted HDD at r = 0.998. Every indicator uses only what was known by about 1 November: October AO and NAO from ERA5; October Eurasian snow extent and its rate of advance from ERA5 snow depth (40–70°N, 0–180°E); the Gulf of Alaska September–October sea surface temperature; the September–October equatorial wind at 30 and 50 hPa; whether last winter had a major stratospheric warming; last winter's HDD departure; and October's own. El Niño strength is the December–February Niño 3.4 anomaly, which seasonal models forecast well by October. Significance comes from a control of 2,000 random predictors; forecast skill is mean-squared-error skill for winters 1970/71–2025/26, each predicted only from earlier winters. Not tested: the solar cycle.