We're About To Have A RARE Winter... | Ryan Hall, Y'all

The Gist

A stronger than 90 percent chance of a very strong El Nino points to a historic winter shift across North America for 2026 to 2027. The southern tier will face frequent storm activity and heavy rain, while the northern tier experiences mild temperatures and limited snow.

Quick Overview

NOAA forecasts a greater than 90 percent chance of a very strong El Nino for the 2026 to 2027 winter, with a 69 percent chance of exceeding every recorded El Nino since 1950. This pattern displaces the jet stream further south, resulting in stormy conditions across the Gulf Coast, Texas, and the Southeast, while leaving the northern states in a barely there winter. California faces a delayed start to the season followed by frequent Pacific storm threats, and the East Coast remains a coin flip depending on whether cold Arctic air drops south in time.

Key Points: NOAA data indicates a greater than 90 percent chance of a very strong El Nino for the fall and winter of 2026 to 2027. There is a 69 percent chance that this El Nino will exceed the historic intensity of the 1982 to 1983 event, which holds the current record peak index of 2.40 degrees Celsius. The southern storm track delivers frequent heavy rain and potential severe weather from Texas through the Gulf Coast and into Florida. Northern tier states including Minnesota, Wisconsin, and Michigan face a barely there winter with over 50 percent odds of above-normal temperatures. Washington, D.C. and Baltimore experienced massive snowfall variations during past El Nino events, ranging from 0.1 inches in 1997 to 1998 up to 56.1 inches in 2009 to 2010. California can expect a quiet early winter followed by a series of Pacific storm systems that bring heavy rain to the coast and significant snow to the mountains. The winter storm battleground zone spanning Oklahoma, Arkansas, Tennessee, and the Carolinas creates a sleeper zone for major unexpected snow or ice events if cold air aligns with moisture.

Context: El Nino events alter global atmospheric circulation by warming the tropical Pacific Ocean, shifting jet stream tracks, and fundamentally changing seasonal temperature and precipitation averages across the United States. Weather forecasters analyze these anomalies months in advance to anticipate how storm paths and cold air outbreaks will affect regional snowfall and rainfall.