Environment and Natural Resources Service
FAO Research, Extension and Training Division
18 March 2002
El Niņo1 is a coupled atmospheric and oceanic phenomenon; predictions are based on several independent observations, including the following:
Indications for a warm episode in the Tropical Pacific (or El Niņo proper) were first noted in August 2001. With oscillations, the evolution towards a warm episode in the tropical Pacific continued until February 2002. Several of the atmospheric indices indicate that El Niņo/ Southern Oscillation (ESN) conditions have not developed to the point that guarantees sustained growth of the event.
To estimate future ENSO conditions, a common practice is to compare different reputable models that currently represent the state-of-the-art as far as dynamical and statistical ENSO prediction systems are concerned; they are useful guidance up to about nine months ahead.
Of 11 models, five show a transition to warm conditions between about May and September 2002. However, at both 5 months (July) and 8 months lead (October), the majority of models favour Neutral conditions. Furthermore, the amount of warming shown across the various predictions is not as strong as that shown last month, and it is in no way comparable to the latest strong 1997-98 event.
For the time being, the interpretation of El Niņo indicators thus remains mixed. Several leading meteorological services (e.g. the US National Oceanic and Atmospheric Administration -NOAA- and the Australian Bureau of Meteorology -BOM-) caution that it is still too early to predict the magnitude and the duration of the potential 2002-2003 El Niņo.
1For a general description of the El Niņo phenomenon, please refer to the FAO website: An el Niño primer
For the latest El Niño updates, please see: