El Niño Conditions Are Growing Stronger

El Niño Conditions Are Growing Stronger
  • Credit:

    NASA Earth Observatory image by Jesse Allen, using Jason-2 data provided by Akiko Kayashi and Bill Patzert, NASA/JPL Ocean Surface Topography Team. Caption by Mike Carlowicz.

When scientists declared in March 2015 that El Niño conditions had developed in the Pacific Ocean, the consensus was that the event was too weak and too late to have much effect on North America. But in the past several months, warm water has been sloshing from the western Pacific toward the Americas and El Niño has strengthened. Surface waters have grown significantly warmer in the central and eastern Pacific, and conditions have become somewhat cooler and drier in the west. By the end of July 2015, scientists at NASA and other agencies started to see some similarities between current conditions and the development of the potent El Niño event of 1997–98.

“We have not seen a signal like this in the tropical Pacific since 1997,” said Bill Patzert, a climatologist at NASA’s Jet Propulsion Laboratory. “It’s no sure bet that we will have a strong El Niño, but the signal is getting stronger. What happens in August through October should make or break this event.”

The maps on this page provide NASA’s view of Pacific Ocean conditions. At the top of the page, you can see snapshots of the averaged sea surface height anomalies at four different moments since March 2015. Shades of red indicate where the ocean stood above normal sea level because warmer water expands to fill more volume (thermal expansion). Shades of blue show where sea level and temperatures were lower than average (thermal contraction). Normal sea-level conditions appear in white. The maps are based on altimetry measurements made by the OSTM/Jason-2 satellite and analyzed by scientists at NASA’s Jet Propulsion Laboratory.

Below you can see an animation of the same data from January 1 through July 31, 2015. Note how pulses of warmer water seem to move from west to east across the Pacific basin. There is a subtle signal in January, and then increasingly stronger pulses in March, May, and July.

The pulses of warmer water moving across the ocean are Kelvin waves. Sea level is naturally higher in the western Pacific; in fact, it is roughly 40 to 50 centimeters (15-20 inches) higher near Indonesia than off of Ecuador. Much of this difference is due to tropical trade winds, which predominantly blow from east to west across the Pacific Ocean, piling up the water near Asia and Oceania. When those trade winds ease and bursts of wind come out of the west, warm water from the western Pacific sloshes east in vast and deep waves and evens out sea level a bit. As the warm water piles up in the east, it suppresses the natural upwelling that usually keeps waters cooler along the Pacific coasts of the Americas.

The seas and skies have been doing just that in 2015. According to observations compiled by the National Oceanic and Atmospheric Administration (NOAA), at least three sizable west wind bursts have occurred in the Pacific since March, and each came shortly before a Kelvin wave rolled across the basin. Those waves have raised water temperatures in the central and eastern Pacific by as much as 1.6 degrees Celsius (2.9° Fahrenheit) above normal, making for a “strong” El Niño. The warmers waters off the west coast of the Americas have led to warmer and more humid weather ashore, as well as soaking bursts of rain. At the same time, Indonesia and other parts of the western Pacific have been unusually dry.

“Sea surface temperatures in the eastern Pacific have been waxing and waning,” Patzert said. “Right now they are waxing.” But will sea surface conditions and winds amplify the warming signal and produce an El Niño to rival 1997–98?

Below you will find a comparison of sea surface height in the Pacific as measured at the end of July in 1997 and 2015. The left-side measurements come from the TOPEX/Poseidon mission, while the right side is from Jason 2. Comparing the two years, 1997 seems slightly less intense. But trade winds collapsed and the eastern Pacific warmed dramatically from August through November 1997, setting the stage for a turbulent winter that brought flooding rains and landslides across the West Coast of North and South America. (Click here to see an animation of 1997 conditions compared to 2015.)

“This El Niño is getting billed as the ‘great wet hope.’ Many people in the American West are looking to El Niño to save them from drought,” Patzert noted. But he cautioned that “1997 was mayhem,” and drenching rains on a parched landscape are just as hazardous as a drought.

El Niño typically peaks between December and April, so only time will tell if this event will be potent. Many of the models and observations suggest it will be, but other factors such as the “warm blob” in the North Pacific and the apparent shift in the Pacific Decadal Oscillation could affect further development.

“With hopes for drought relief running so high in California, it can’t be stressed enough that El Niño shifts the odds but doesn’t guarantee the roll of the meteorological dice in any particular winter,” wrote meteorologist and blogger Bob Henson.

Scientists from NASA’s Goddard Space Flight Center and other institutions recently found that California has accumulated a “rain debt” of about 50 centimeters (20 inches) between 2012 and 2015. That is the amount that would normally fall in an entire year in the state.

And even if the rains come, they do not necessarily solve drought problems in areas that rely on snow pack for summer supplies. “It took a long time to get into this drought,” Patzert added, “and it is more of a systemic problem than just a lack of rain or snowfall.”

Images & Animations


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  • Data Date:

    January 0, 2015 - July 0, 2015
  • Visualization Date:

    August 3, 2015
  • Sensor(s):

NASA - National Aeronautics and Space Administration