Climate Central

Climate Central’s Monthly Briefing Highlights from January 2026

What do experts say?

Dr. Zachary Labe, climate scientist at Climate Central, said:
“Winter isn’t gone – it’s changing. It can still get dangerously cold, but there are fewer freezing nights over time. Cold outbreaks still happen, but they are becoming shorter. Extreme cold still shows up, but it’s not like before.”

“Although the eastern U.S. was unusually cold and snowy by recent standards in January, the West was strikingly warm with record-low snowpack, a potential warning sign for drinking water supplies for the remainder of the year.”

Global Climate

U.S. Climate

Climate Moment of the Month with Tom

By Tom Di Liberto, media director at Climate Central

Starting February 1, there’s a new official way the National Oceanic and Atmospheric Administration (NOAA) is tracking and measuring El Niño and La Niña! Moving forward, NOAA will be using the Relative Oceanic Niño Index (RONI) to designate the occurrence and strength of past events and in all predictions for future El Niño-Southern Oscillation (ENSO) events. This big news rewrites the history of ENSO events in the modern-era, but you might be wondering, why the change? Let’s jump in.

The simple answer is climate change. The traditional method for measuring and tracking ENSO, called the Oceanic Niño Index (ONI), is calculated by determining the sea surface temperature difference from the 30-year average across the Niño 3.4 region in the east-central tropical Pacific Ocean. That calculation is heavily dependent on which30-year period is chosen. In a stable climate, the choice of period does not matter. But our climate is changing, and the waters across the tropical Pacific are warming. And even with updating the 30-year time period every five years, NOAA’s ONI struggles to keep pace.

At a fundamental level, the ONI also does not capture the contrast in ocean temperatures between the east-central Pacific Ocean and the rest of the tropical Pacific that sets off the atmospheric dominos that leads to the global impacts felt during El Niño and La Niña.

The solution? The RONI, which compares the ENSO region of the tropical Pacific to the global tropics (details about how RONI is calculated are available in the link above). This reduces the reliance on a 30-year climate base period, and the impact of rising ocean temperatures due to climate change, while also better reflecting the ocean-atmosphere mechanisms that drive developing El Niño and La Niña events.

So as 2026 progresses and the tropical Pacific veers from La Niña to a potential El Niño, make sure you ask one very important question. “Hey, what ENSO index are you using? RONI or ONI?”

CS: The Monthly Climate Brief - January 2026 Graphic 3

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Methodology

Global and U.S. climate statistics are provided by NOAA’s National Centers for Environmental Information (NCEI), including through the Climate at a Glance tool. All climate regions and divisions follow the standard definitions established by NOAA NCEI. Data is also provided by the Applied Climate Information System (ACIS) using ThreadEx, which is developed, maintained, and operated by NOAA’s Regional Climate Centers. We recognize that climate ranking statistics can vary slightly between datasets, and there are higher uncertainties in temperature data prior to 1900. 

Drought information is available through the U.S. Drought Monitor, and western U.S. snowpack data is provided by the USDA National Water and Climate Center. Weekly and seasonal temperature and precipitation outlooks are from the NOAA Climate Prediction Center. Sea ice data statistics are from the National Snow and Ice Data Center’s Sea Ice Index v4. Carbon dioxide concentration data is from the NOAA Global Monitoring Laboratory

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