As climatological summer and the Atlantic hurricane season begin on June 1, scientists are carefully monitoring sea-surface temperatures in the tropical Pacific Ocean for a potential El Niño event. An El Niño occurs when warmer-than-average waters start to form in the eastern Pacific Ocean, specifically near the equatorial latitudes. Easterly winds (blowing from the east) typically move warmer water to the western Pacific (near Indonesia), permitting cooler water to upwell to the surface in the east (near South America). When these winds are weaker, or if they reverse direction, the warm water stays in the eastern Pacific. This difference in sea surface temperatures and winds creates a new dynamic between the ocean and atmosphere, distinctly affecting weather patterns across the world. No two El Niño events are alike; they vary in magnitude and location of the largest temperature anomalies. El Niño events can be classified as Strong, Moderate or Weak.
Scientists monitor the oceans through a network of buoys and formulate a forecast for El Niño events. Figure 1 shows current sea surface temperature anomalies globally, indicating a growing positive departure from normal in the eastern equatorial Pacific. An El Niño has yet to be declared, as conditions need to be present for three consecutive months to be considered an official event. NOAA has launched a blog to discuss this apparently unfolding event. Confidence is steadily increasing that an El Niño will occur this year.

Figure 1. Sea Surface Temperature (SST) anomalies for May 29, 2014. NOAA/NESDIS.

Figure 2. Time series of New Jersey average summer temperatures from 1951-2013. Red bars indicate years with an El Niño event. Black line indicates 5-year moving average.

Figure 3. Distribution of average summer temperatures from 1951-2013, representing percentage of El Niño summers falling within each tercile.

Figure 4. Time series of New Jersey total summer precipitation from 1951-2013. Red bars indicates years with an El Niño event. Black line indicates 5-year moving average.

Figure 5. Distribution of total summer precipitation from 1951-2013, representing percentage of El Niño summers falling within each tercile.
- Current Analysis - http://www.cpc.ncep.noaa.gov/products/precip/CWlink/MJO/enso.shtml
- A more in-depth explanation of El Niño - http://www.pmel.noaa.gov/tao/elnino/el-nino-story.html
- FAQ about the El Niño - http://www.cpc.ncep.noaa.gov/products/analysis_monitoring/ensostuff/ensofaq.shtml#ENSO
- More forecasting tools - http://iri.columbia.edu/our-expertise/climate/forecasts/enso/