Breaking News
CPC will begin to use the RONI data to calculate the sst anomalies. I think our friend
LarryWx was the one promoting this for a long time and here it is starting on Febuary 1.
https://www.weather.gov/media/notificat ... ve_ONI.pdf
Public Information Statement Implementing a Relative Oceanic
Niño Index effective February 1, 2026
The National Centers for Environmental Prediction (NCEP) Climate
Prediction Center (CPC) informs the public of the shift to a Relative
Oceanic Niño Index for the official monitoring and prediction of the El
Niño-Southern Oscillation (ENSO) phenomenon, effective February 1, 2026.
ENSO is the leading pattern of year-to-year climate variability, and
plays an important role in subseasonal to seasonal variations in
temperature, precipitation, storm tracks, hurricane activity, and other
impactful variables in the weather-climate system.
When implemented, NCEP CPC will define El Niño (La Niña) as a relative,
positive (negative) mean SST anomaly of 0.5 degrees C or greater over 3
consecutive months in the Niño 3.4 region of the central Pacific Ocean (5
degrees N to 5 degrees S and 120 degrees W to 170 degrees W). This
anomaly is computed by subtracting the average SST anomaly of the global
tropics (20 degrees N to 20 degrees S) from the Niño 3.4 regional
anomaly. After the subtraction, the relative index is rescaled to match
the amplitude of the traditional index.
The Relative Oceanic Niño Index (RONI) is defined as the three month
running average of the relative Niño 3.4 index. Historical El Niño and
La Niña events will be categorized based on this index, specifically when
there are five or more consecutive, overlapping three-month seasons where
the RONI is greater than 0.5C (El Niño) or less than -0.5C (La Niña).
The RONI is visually very similar to the traditional ONI, so users can
use it in the same way as they would the traditional ONI.
This proposed change will have two primary benefits for ENSO monitoring
and prediction: 1) the relative sea surface temperature index better
identifies current and past El Niño and La Niña events because it is less
sensitive to the chosen base climatology period. This allows for
comparison of events across the lengthy climate record. 2) A relative
index is more related to changes in rainfall over the tropical Pacific
than the traditional index. Over the past year, the relative SST index
was better aligned with the intensity of rainfall anomalies and
circulation changes associated with the ENSO phenomenon. It is the
change in tropical rainfall and heating that ultimately drives the
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