With climatologists uncertain how powerful the impending El Nino will be, California residents need to be prepared for anything from light showers - which this UCI student takes in stride - to serious deluges. Steve Zylius / UCI

Forecast: cloudy

Predicting intensity, impact of this winter’s El Nino complicated by unprecedented confluence of weather anomalies

El Nino is officially upon us, and some scientists are describing it as a monster climatic event.

But will it be as powerful as similar conditions in the early 1980s and late 1990s? Will it deliver much-needed rain to California’s aquifers and snow to its mountains? Does the intensity of this year’s event have something to do with global climate change? The scientific community – as well as the public – is asking these questions and more, but answers are elusive.

Climatologists are having difficulty predicting what will happen because this year’s El Nino is unlike any other. The intense ocean warming we are witnessing now is an unprecedented second El Nino in a single year. The first, in the central Pacific Ocean, flared up and died down months ago. And our current El Nino is overlapping a huge mass of warm water extending from Alaska to Baja California known as the “Pacific blob.”

“This year there’s a battle between the Pacific blob and a strong traditional El Nino. It’s a different phenomenon. We can’t use past events to help us predict what’s going to happen,” says University of California, Irvine climatologist Jin-Yi Yu.

Technically speaking, an El Nino is an increase of tropical Pacific sea surface temperatures by 0.5 degrees Celsius or more for at least three months. Historically happening every two to seven years, it has effects potentially felt around the Pacific basin, from drier conditions in Australia and Indonesia to increased rainfall in the southern United States. Atmospheric scientists use the acronym ENSO (El Nino Southern Oscillation) when discussing the phenomenon.

Experts had been getting pretty good at predicting El Nino events, Yu says: “The ’82-’83 one was a big wake-up call for the scientific community, because we realized how strong the impact could be. From 1982 to 1997, the year of the next big El Nino, we were able to learn a lot, and we developed computer models that could tell us if another one was coming up to a year before it happened. It was a very successful story in the scientific community.”

But as the 21st century has progressed, experts have found it harder to predict both the onset of such conditions and their impact on North America. “We noticed that the El Nino model prediction skill dropped in the early part of the century, but we didn’t know why,” Yu says. “It turns out that what we’ve observed in the past 10 or 15 years is another type of climate phenomenon. It looks like an El Nino, but it’s different from the one we used to know.”

The traditional type originates in the eastern Pacific Ocean along the South American coast. Time-lapse maps would show the warmer water extending to the west along the equator and moving up toward North America.

A climate data map from January 1997 through July 1999 shows the occurrence of a “traditional” eastern Pacific El Nino. Jin-Yi Yu / UCI

In contrast to this classic El Nino, the past decade and a half has seen similar but weaker conditions forming in the central Pacific instead, at the intersection of the equator and the international date line. These newly observed El Ninos don’t affect the weather in California to the same degree as the eastern Pacific ones. They frequently die down, and they’ve consistently delivered less rain to the southern U.S. Yu says the prevalence of this new type of El Nino may even be a factor contributing to California’s ongoing drought.

A central Pacific El Nino can be seen growing and shrinking on a climate data map spanning July 1977 to April 1978. Jin-Yi Yu / UCI

In March, the National Oceanic & Atmospheric Administration did project a central Pacific El Nino. Like others before it, this one was weak and short-lived, lasting only from April to June. Through the first half of 2015, it appeared that an emerging trend of inconsequential El Nino events was holding fast.

But this year is different. It’s the first return of an eastern Pacific El Nino since 1997-98. “We’re having a rare double event, a central Pacific El Nino followed by an eastern Pacific one,” says Yu, who’s credited with identifying and naming the two varieties in a 2007 research paper. “The question now is whether the earlier central Pacific El Nino has made the current eastern Pacific event stronger or weaker. … We just don’t know.”

Compounding scientists’ uncertainty is a third large-scale climate phenomenon called the Pacific blob, an area of warmer-than-normal water along the North American coast from Alaska to Baja California. Swimmers and surfers in California have been enjoying more temperate ocean water later in the season this year, and some unfamiliar marine life has been found near the shore. Warmer ocean water also affects the atmosphere.

“The Pacific blob has been in place for quite some time, and people believe that’s why we’ve been having this drought for so long,” says atmospheric scientist Gudrun Magnusdottir, chair of UCI’s Department of Earth System Science. “Warmer ocean water tends to put a ridge of high pressure in place, and that diverts storms that could potentially deliver water to drought-stricken areas.”

Yu says the addition of the blob to the mix is another reason why climatologists seeking to predict what this year’s El Nino might bring can’t extrapolate from the 1997-98 event.

 With his powers of prognostication diminished, Yu is forging ahead on a new line of inquiry – what’s behind the general shift from eastern Pacific to central Pacific El Ninos. “If it were because of global warming, I think the traditional form of El Nino would be gone forever or would only come back occasionally,” he says.

But Yu doesn’t think the switch can be attributed to global warming. “I argue that it’s due to something that happened in the Atlantic Ocean,” he says. Yu is referring to the Atlantic Multidecadal Oscillation, a roughly 80-year ocean warming and cooling cycle that has cascading effects throughout the world.

“In the last 10 to 15 years, the Pacific Ocean is more a slave to what’s been happening in the Atlantic. So I believe the change in El Nino that we’re seeing is not due to global warming – although I cannot exclude that possibility. El Nino’s location change will switch back by nature itself. At some point, it’s going to come back to the eastern Pacific. That, I project, is still a decade or more in the future.”

Yu says it’s still important to diligently track El Nino conditions. Only by doing so will we be able to manage water resources, protect infrastructure and prepare for flooding if this or future El Ninos bring significant rainfall to California.