This vast pool of warm water is thought to set off a chain reaction that can affect jet stream and weather patterns around the world, especially in the winter months in the northern hemisphere. El Niño is sometimes referred to as ENSO for El Niño–Southern Oscillation. The Southern Oscillation is a seesaw of air pressures on the eastern and western halves of the Pacific. See El Niño Pattern chart.
Q. What is La Niña?
A. La Niña is essentially the opposite of El Niño. La Niña refers to the periodic cooling of ocean surface temperatures in the central and east-central equatorial Pacific that occurs every 3 to 5 years or so. The cool water can suppress rain-producing clouds, which leads to dry conditions. See La Niña Pattern chart.
Q. What do the terms “El Niño” and “La Niña” mean?
A.Peruvian fishermen first noticed the effects of a new El Niño at Christmas time, when storminess off the coast reduced the supply of fish. “El Niño” is Spanish for “the boy child,” and is used to refer to the Baby Jesus. The name La Niña (“the girl child”) was coined to deliberately represent the opposite of El Niño.
Q. How do these weather events affect winter weather?
A. Because even the most dedicated scientists do not thoroughly understand El Niño and La Niña (we do not know, for instance, why the trade winds suddenly die down and allow the warm water pool to move eastward), we can only describe certain tendencies in the weather.
In the past, El Niño has often brought heavy rains to southern California and to a portion of the South from Atlanta to Cape Hatteras; it can bring relatively mild winter temperatures to the northern third of the country. However, these effects are not consistent in every El Niño event on record.
Conversely, the stronger the La Niña, the more severe the droughts. The La Niña of 2009, for example, created severe drought in much of the world, causing an agricultural crisis in some areas.