I wrote about El Niño and New Jersey weather recently. Here's a follow-up with information from State climatologist John Krasting, an extension specialist at Rutgers and an affiliate of the Rutgers Climate and Energy Institute.
Krasting’s advice is monitoring rather than prediction. It is plausible New Jersey sees an active and damaging winter. It is also possible the jet pattern shifts, individual storms miss the coast, or temperatures favor rain over snow in ways that change the impact.
The tropical Pacific is in an exceptionally strong El Niño, and it is expected to persist into early 2027. El Niño is a naturally occurring process in the tropical Pacific where the trade winds relax and the upper ocean warms. The warming covers a large enough area to influence the jet stream and weather patterns around the world. Scientists call those long-distance connections teleconnections, and they use past events and computer model simulations to identify regional patterns that become more likely during El Niño.
The cycle is part of the El Niño Southern Oscillation, or ENSO. El Niño typically occurs once every two to seven years. La Niña is the opposite phase, with cooler-than-average sea surface temperatures in the tropical Pacific, and the cycle back and forth is the largest driver of year-to-year weather variability around the world. Last year was La Niña.
Krasting does not predict snow or temperatures for New Jersey from El Niño alone. His framing is deliberate: “Every El Niño has its own ‘personality,’ and only time will tell how it will ultimately impact New Jersey.”
New Jersey enters this winter with less buffer than usual. A powerful, early-season nor’easter in late September caused significant erosion, the worst since Superstorm Sandy in some locations. The New Jersey Department of Environmental Protection surveyed 81 reaches after the storm and found major beach or dune erosion in 10 of them,
Another nor’easter this weekend is bringing rain to NJ, hail on Thursday and snow to areas north of the state.
The number to watch is not absolute ocean temperature; it is the anomaly, how far above the rest of the tropics the Niño-3.4 region has warmed. NOAA now tracks this with the Relative Oceanic Niño Index, or RONI, which compares Niño-3.4 to the rest of the tropics to isolate the ENSO signal from background warming. By that measure, an El Niño begins at 0.5°C above the rest of the tropics. Rutgers reported NOAA sea surface temperature anomalies of 2.5°C in the tropical Pacific in early November. In its November 12 discussion, NOAA put Niño-3.4 at +2.5°C, with even larger anomalies farther east at +3.6°C in Niño-3 and +4.4°C in Niño-1+2.
At 2.0°C and above, NOAA's official top category is very strong. “Super El Niño” is the informal name for the same threshold. Only five such events had occurred since 1965 before this one, which makes 2026 to 2027 the sixth.
An earlier November outlook put the chance this becomes the strongest since 1950 at greater than 80 percent. The November 12 update puts that chance at about 60 percent, while still expecting a strong to very strong event through winter. That revision is normal in seasonal forecasting. The ocean is very warm, the exact placement in the historical ranking is uncertain.





