不良研究所

The Mystery of El Ni帽o

不良研究所 Scientists on Past, Present, and Future Unknowns of El Ni帽o

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When the Pacific Ocean sloshed warm water back toward Peru in the 1500s, the country鈥檚 fisheries collapsed around Christmas time. A name was born: 鈥淓l Ni帽o: The Christmas Child.鈥 

鈥淚t鈥檚 the little child of Christ who is causing problems,鈥 said 不良研究所 Atmospheric Science Professor

El Ni帽o is expected to be causing problems, again, from now and through this winter. 不良研究所 experts weigh in on the knowns and unknowns of what California and the rest of the world may expect.

What about California?  

Even though global temperatures increase with El Ni帽o, impacts are not the same everywhere. The West Pacific, like Southern Asia and Australia, may experience drought, while the East Pacific, like Peru and Southern California, may experience a very wet winter. 

This Eastern Pacific coast normally experiences upwelling of cold, nutrient-dense water from powerful winds pushing the water away from the coast into the Pacific. But when these trade winds weaken, warm water is pushed back toward the coast and results in powerful storms. This is El Ni帽o, while La Ni帽a occurs when these winds strengthen.  

Global impacts of El Nino, showing a drier Oregon and wetter Southern California
How El Ni帽o commonly impacts the globe across seasons (Courtesy NOAA).

The warm water location change is linked to where moist, hot air rises in worldwide convection currents, which can cause major shifts in storm structure and dynamics across the globe. 

But although Southern California is forecasted for rain, the Pacific Northwest is expected to experience drying, leaving the Central Valley right in the middle. 

鈥淭he effects sort of miss us, in a sense,鈥 Faloona said. 鈥淲e鈥檙e kind of in this transition zone.鈥 

However, the Central Valley should receive more water from increased snowfall in Southern California mountain ranges. Good news for California skiers and snowboarders.

But why? 

The believed that El Ni帽o was caused by angry sea gods. Today, El Ni帽o is still mystifying. 

鈥淓very 2-7 years, the winds seem to just weaken in the summertime,鈥 said Faloona. 鈥淚 think it鈥檚 very mysterious how it evolves.鈥 

What triggers El Ni帽o is a hot topic of research, and is something that , 不良研究所 assistant professor of Computer Science, is hoping to dive deeper into over the next few years.

鈥淓l Ni帽o is such an interesting phenomenon because it is effectively the ocean talking to the atmosphere and having this global conversation,鈥 Sonnewald explained. 鈥淵ou can鈥檛 just look at the atmosphere; you can't just look at the ocean. You need to look at both.鈥 

With trade winds, atmospheric convection currents, global storm structure, oceanic energy, and planetary movement all interacting with each other, it is hard to pin down cause and effect. 

鈥淓verything is coupled,鈥 said Faloona. 鈥淚t鈥檚 a little bit of a chicken and egg.鈥 

El Nino and La Nina cycles since 1950
The El Ni帽o and La Ni帽a oscillation from 1950 through 2023 (Courtesy NOAA).

A mysterious future 

El Ni帽o increases global temperatures overall, which can aggravate the effects of climate change and result in record high temperatures. With climate change, El Ni帽o鈥檚 effects may also be more intense. 

This dynamic is a tricky one to study. Although historical records of El Ni帽o go back to 2,200 B.C, there are only around 12 fully comprehensive observations of El Ni帽o in the past 40 years. 

鈥淚t鈥檚 hard to say anything about a sample of 12,鈥 Faloona said. 鈥淚t鈥檚 easy to find something universal and be fooled by the low number of observations.鈥 

This lack of data is why scientists rely so much on models. Sonnewald and her student, Zouberou Sayibou, worked with climate models to understand how El Ni帽o will change under different climate and socio-economic pathways. 

鈥淯nfortunately, we don鈥檛 have data from the future. So we have to use models,鈥 said Sonnewald. 

Sonnewald and Sayibou鈥檚 model analysis suggests that El Ni帽os may increase in severity under climate change. Temperature anomalies like marine heat waves may also increase with the combination of El Ni帽o heating and climate change. Still, with the complexity of El Ni帽o鈥檚 patterns and the unknowns behind the phenomenon, much is still left to discover. 

鈥淚t鈥檚 very uncharted territory,鈥 Sonnewald said. 鈥淏ut I think we as a scientific community are ready for it. I鈥檓 excited.鈥 

Present predictions 

Predicting when El Ni帽o will occur is also a mystery. However, once the events begin to form, scientists can predict intensity by taking the average temperature in a specific band of increasingly warm water around the equator. This temperature becomes the Oceanic Ni帽o Index (ONI).

This index not only predicts how intense the event will be, but also how many people will be affected by El Ni帽o. As of now, more people may be food insecure this winter because of reduced crop yields due to El Ni帽o. 

鈥淲e need to be able to tell local communities what they need to prepare for,鈥 said Sonnewald. 

But even if scientists know possible global impacts, local weather predictions under El Ni帽o are difficult. A small anomaly 鈥渨obble鈥 can be a big deal for places like California, said Sonnewald. For example, La Ni帽a tends to average toward a drier Southern California, yet that region experienced flooding during last year鈥檚 La Ni帽a.

鈥淚t is a chaotic system,鈥 said Faloona. 鈥淭iny, tiny changes can create a very different future for weather.鈥 

 


Malia Reiss is a science news intern with 不良研究所 Strategic Communications. She studies environmental science and management at 不良研究所.

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