El Niño: Facts, news, features and articles about the climate cycle that impacts weather patterns around the globe

El Niño conditions occur every three to five years but may come as frequently as every two years or as rarely as every seven years. Typically, El Niño events occur more frequently than La Niña conditions. Each event usually lasts nine to 12 months. They often begin to form in spring, reach peak strength between December and January, and then decay by May of the following year.

Scientists still don't fully understand what triggers an El Niño cycle. Not all El Niño events are the same, nor do the atmosphere and ocean always follow the same patterns from one El Niño to another.

To forecast El Niño, scientists monitor several regions across the Pacific.

"You have to think of each region as an ocean sloshing around," said Neville Sweijd, director of the Alliance for Collaboration on Climate and Earth Systems Science (ACCESS) in South Africa. "Sometimes it sloshes to one side, and sometimes it sloshes to the other. That's El Niño and La Niña."

Experts "monitor the average sea-surface temperature in each region and use that to form a model," he told Live Science. "The models will then predict the likelihood of the manifestation."

In normal, non-El Niño conditions, trade winds blow toward the west across the tropical Pacific, away from South America. These winds pile up warm surface water in the western Pacific so that the sea surface is about 1.5 feet (0.5 meters) higher near Indonesia than it is off the shore of Ecuador. Higher sea-surface temperatures cause water levels to expand and rise and also shift rainfall from the land to the ocean.

In a non-El Niño year, the sea-surface temperature is also about 14 degrees Fahrenheit (8 degrees Celsius) warmer in the western Pacific. Cooler ocean temperatures dominate off the coast of northwest South America, due to an upwelling of cold water from deeper levels.

Forecasters declare an official El Niño when they see both ocean temperatures and rainfall from storms veer to the east. Experts also look for prevailing trade winds to weaken. These changes set up a feedback loop between the atmosphere and the ocean that boosts El Niño conditions.

During El Niño, the trade winds weaken in the central and western Pacific. Surface water off South America warms up because there is less upwelling of the cold water from below to cool the surface. The clouds and rainstorms associated with warm ocean waters also shift eastward. The warm waters release so much energy into the atmosphere that weather changes all over the planet.

El Niño creates stronger wind shear and more stable air over the Atlantic, which makes it harder for hurricanes to form there. However, the warmer-than-average ocean temperatures boost eastern Pacific hurricanes, contributing to more active tropical storm seasons.

Strong El Niño events are also associated with above-average precipitation in the southern United States. The cloudier weather typically causes below-average winter temperatures in that part of the country, while temperatures tilt warmer than average in northern U.S. states. Rainfall is often below average in the Ohio and Tennessee valleys and the Pacific Northwest during El Niño, according to NOAA.

Record rainfall often strikes Peru, Chile and Ecuador during El Niño.

El Niño also affects precipitation in other areas, including Indonesia and northeastern South America, which tend toward drier-than-normal conditions. Temperatures in Australia and Southeast Asia run hotter than average. El Niño-caused drought can be widespread, affecting southern Africa, India, Southeast Asia, Australia, the Pacific Islands and the Canadian prairies.

Unlike El Niño, La Niña events are characterized by a sustained cooling effect around the equator and eastern tropical Pacific. This often results in stronger and more frequent hurricanes across North America and can lead to heavy flooding in many Pacific Island nations, as well as droughts along the west coast of South America.