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Summary of ENSO Model Predictions

16 June 2010

> Note on interpreting model predictions
> Figure of Nino3.4 SST prediction
> Table of Nino3.4 SST predictions
> Discussion of current predictions
> Summary of predictions, last 22 months
> Individual Model View, last 22 months
> Additional information on models
> Notes on the data

Note on interpreting model predictions

The following graph and table show predictions made by dynamical and statistical models for SST in the Nino 3.4 region for nine overlapping 3-month periods. Note that the expected skills of the models, based on historical performance, are not equal to one another. The skills also generally decrease as the lead time increases. Thirdly, predictions made at some times of the year generally have higher skill than predictions made at other times of the year--namely, they are better when made between June and December than when they are made between February and May. Differences among the predictions of the models reflect both differences in model design, and actual uncertainty in the prediction of the possible future SST scenario.

Table 1. Predicted SST Anomalies (deg C) in the Nino 3.4 Region

  Seasons (2010-2011)
Model JJA JAS ASO SON OND NDJ DJF JFM FMA
Dynamical models
NASA GMAO model -2 -2.4 -2.6 -2.6 -2.6 -2.5 -2.4 -2.1 -1.8
NCEP Coupled Fcst Sys model -1 -1 -1 -1.1 -1.3 -1.4 -1.3    
Japan Met. Agency model -0.6 -0.7 -0.7 -0.8 -0.8        
Scripps Inst. HCM -0.1 -0.1 -0.1 -0 0.1 0.1 0.2 0.3 0.4
Lamont-Doherty model -0.3 -0.5 -0.5 -0.6 -0.8 -0.9 -1 -0.8 -0.6
POAMA (Austr) model -0.8 -0.8 -0.8 -0.8 -0.8 -0.8      
ECMWF model -0.6 -0.8 -0.9 -1          
UKMO model -1.7 -1.7 -1.4 -1.2          
KMA (Korea) SNU model -0.7 -0.8 -0.7 -0.6 -0.5 -0.4 -0.3 -0.3 -0.3
ESSIC Intermed. Coupled model -0.8 -1.1 -1.3 -1.5 -1.6 -1.5 -1.3 -1.1 -0.9
ECHAM/MOM -0.5 -0.7 -0.9 -1 -1        
COLA ANOM -0.3 -0.5 -0.7 -0.9 -1.1 -1.1 -1 -0.8 -0.6
MÉTÉO FRANCE model -1 -1 -0.7 -0.5 -0.4        
Japan Frontier Coupled model -1.6 -1.7 -1.7 -1.7 -1.8 -1.9 -2 -2 -2
COLA CCSM3 model -0.5 -0.5 -0.5 -0.5 -0.5 -0.4 -0.3 -0 0.3
Average, dynamical models -0.8 -1 -1 -1 -1 -1.1 -1 -0.9 -0.7
Statistical models
NCEP/CPC Markov model -0.4 -0.5 -0.6 -0.6 -0.6 -0.6 -0.5 -0.5 -0.4
NOAA/CDC Linear Inverse -0.3 -0.5 -0.6 -0.7 -0.7 -0.7 -0.8 -0.7 -0.7
NCEP/CPC Constructed Analog -0.2 -0.4 -0.5 -0.7 -0.9 -1.1 -1.2 -1.1 -0.8
NCEP/CPC Can Cor Anal 0.1 0.1 0.1 0 -0.1 -0.2 -0.2 -0.1 -0.1
Landsea/Knaff CLIPER -0.1 -0.1 -0 -0 -0 -0 -0 0 0
Univ. BC Neural Network -0.3 -0.4 -0.3 -0.3 -0.2 -0.1 0.1 0.2 0.2
FSU Regression -0.4 -0.4 -0.5 -0.5 -0.5 -0.5 -0.4 -0.3 -0.2
TDC - UCLA -0.4 -0.5 -0.7 -0.9 -1.1 -1.2 -1.1 -0.9 -0.7
Average, statistical models -0.2 -0.3 -0.4 -0.5 -0.5 -0.5 -0.5 -0.4 -0.3
Average, all models -0.6 -0.7 -0.8 -0.8 -0.8 -0.8 -0.8 -0.6 -0.5

Discussion of current predictions

Fifty-seven percent of the set of dynamical and statistical model predictions issued during late May and early June 2010 indicate ENSO-neutral conditions during the June-August season currently in progress, while 43% predict La Nina conditions. However, for the upcoming July-September period these percentages reverse to 39% and 61%, respectively, as La Nina development becomes the more common prediction from that season through the end of 2010. There is some disagreement among models about the ENSO state during the remainder of 2010, with predictions ranging from near-neutral to strong La Nina conditions. At the time of preparing this, the SST observations in the NINO3.4 region indicate borderline La Nina conditions, with an area-averaged weekly anomaly of -0.5 C. Current predictions and observations indicate a probability of about 58% for developing La Nina conditions during the June-August period, increasing to 62% from the August-October period through the end of 2010. Probabilities for returning to El Nino are no more than 1% through the early months 2011.

Summary of predictions issued over last 22 months

The following plots show the model predictions issued not only from the current month (as in the plot above), but also from the 21 months previous to this month. The observations are also shown up to the most recently completed 3-month period. The plots allow comparison of plumes from the previous start times, or examination of the prediction behavior of a given model over time. The first plot shows predictions for dynamical models, the second for statistical models, and the third for all models. For less difficult readability, predictions are shown to a maximum of only the first five lead times. Below the third plot, we provide a mechanism for highlighting the predictions of one model at a time against a background of more lightly colored lines for all other models.




Individual Model View over last 22 months

View individual models here.

Additional information on Models

Dynamical Models Statistical Models
NASA GMAO model NCEP/CPC Markov model
NCEP Coupled Fcst Sys model NOAA/CDC Linear Inverse
Japan Meteorological Agency NCEP/CPC Constructed Analog
Scripps Inst. HCM NCEP/CPC Can Cor Anal
Lamont-Doherty model Landsea/Knaff CLIPER
POAMA (Austr) model Univ. BC Neural Network
ECMWF model FSU Regression
UKMO model TDC - UCLA
KMA SNU (Korea) model  
ESSIC Intermed. Coupled model  
ECHAM/MOM  
COLA ANOM  
MÉTÉO FRANCE  
Japan Frontier Coupled model  

Notes on the data 

Only models producing predictions on a monthly basis are included. This means that some models whose predictions appear in the Experimental Long-Lead Forecast Bulletin (produced by COLA) do not appear in the table.

The SST anomaly predictions are for the 3-month periods shown, and are for the Nino 3.4 region (120-170W, 5N-5S). Often, the anomalies are provided directly in a graph or a table by the respective forecasting centers for the Nino 3.4 region. In some cases, however, they are given for 1-month periods, for 3-month periods that skip some of the periods in the above table, and/or only for a region (or regions) other than Nino 3.4. In these cases, the following means are used to obtain the needed anomalies for the table:

  • Temporal averaging, 
  • Linear temporal interpolation 
  • Visual averaging of values on a contoured map 

The anomalies shown are those with respect to the base period used to define the normals, which vary among the groups producing model predictions. They have not been adjusted to anomalies with respect to a common base period. Discrepancies among the climatological SST resulting from differing base periods may be as high as a quarter of a degree C in the worst cases. Forecasters are encouraged to use the standard 1971-2000 period as the base period, or a period not very different from it.

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