Skip Navigation Links www.nws.noaa.gov 
NOAA logo - Click to go to the NOAA home page National Weather Service   NWS logo - Click to go to the NWS home page
Climate Prediction Center

 
 
HOME > Expert Assessments > ENSO Diagnostic Discussion
 
 
EL NIŅO/SOUTHERN OSCILLATION (ENSO)
DIAGNOSTIC DISCUSSION
issued by
CLIMATE PREDICTION CENTER/NCEP
May 9, 2002
 
NOAA Press Release
 

Warmer-than-normal sea surface and subsurface temperatures were observed throughout most of the equatorial Pacific during April 2002. Sea surface temperature anomalies were up to 2°C warmer than average in the region between the Galapagos Islands and the South American coast, and greater than 1°C warmer than average immediately to the west of 180°W (Fig. 1). Although there was considerable warming in the eastern equatorial Pacific during February-April, which resulted in locally heavy rainfall along the coasts of Ecuador and northern Peru, there was little change in SSTs or subsurface temperature anomalies in regions father west during this period. Consistent with this lack of evolution in the central equatorial Pacific, atmospheric indices for low-level winds, sea level pressure (SOI) and precipitation (OLR) continue to indicate near-normal conditions.

The Madden-Julian Oscillation (MJO) is an important source of variability that can contribute to a more rapid evolution toward El Niņo through related fluctuations in low-level winds and precipitation over the western and central equatorial Pacific. An eastward-propagating oceanic Kelvin wave, initiated by strong MJO activity in late 2001, resulted in the rapid warming that was observed along the coasts of Ecuador and northern Peru in early February. Since that time MJO activity has weakened and there has been no additional significant Kelvin wave activity. Without such activity a slow evolution towards El Niņo conditions is possible through the remainder of 2002.

This assessment agrees well with several coupled model and statistical forecasts, which indicate a gradual warming over the next several months with weak-to-moderate El Niņo conditions by the end of 2002. It is important to add that a weak or moderate El Niņo would feature considerably weaker global impacts than were experienced during the very strong 1997-98 El Niņo.

This discussion is a team effort of NOAA and its funded institutions. Updates of SST, 850-hPa wind, OLR and the equatorial subsurface temperature structure are available on the Climate Prediction Center web page at http://www.cpc.ncep.noaa.gov (Weekly Update).  Forecasts for the evolution of El Niņo/La Niņa are updated monthly in CPC's Climate Diagnostics Bulletin Forecast Forum. To receive an e-mail notification when updated ENSO Diagnostic Discussions are released please send your e-mail address to:

 
Climate Prediction Center
National Centers for Environmental Prediction
NOAA/National Weather Service
Camp Springs, MD 20746-4304
e-mail: vernon.kousky@noaa.gov

NOAA/ National Weather Service
NOAA Center for Weather and Climate Prediction
Climate Prediction Center
5830 University Research Court
College Park, Maryland 20740
Page Author: Climate Prediction Center Internet Team
Page last modified: May 9, 2002
Disclaimer
Information Quality
Credits
Glossary
Privacy Policy
Freedom of Information Act (FOIA)
About Us
Career Opportunities