(Image courtesy of UH Manoa)

MEDIA RELEASE

El Nino wreaks havoc across the globe, shifting weather patterns that spawn droughts in some regions and floods in others. The impacts of this tropical Pacific climate phenomenon are well known and documented.

A mystery, however, has remained despite decades of research: Why does El Nino always peak around Christmas and end quickly by February to April?

Now there is an answer: An unusual wind pattern that straddles the equatorial Pacific during strong El Nino events and swings back and forth with a period of 15 months explains El Nino’s close ties to the annual cycle.

This finding is reported in the May 26, 2013, online issue of Nature Geoscience by scientists from the UH Manoa Department of Meteorology and International Pacific Research Center.

“This atmospheric pattern peaks in February and triggers some of the well-known El Nino impacts, such as droughts in the Philippines and across Micronesia and heavy rainfall over French Polynesia,” says lead author Malte Stuecker.

When anomalous trade winds shift south, they can terminate an El Nino by generating eastward propagating equatorial Kelvin waves that eventually resume upwelling of cold water in the eastern equatorial Pacific.

This wind shift is part of the larger, unusual atmospheric pattern accompanying El Nino events, in which a high-pressure system hovers over the Philippines and the major rain band of the South Pacific rapidly shifts equatorward.

With the help of numerical atmospheric models, the scientists discovered that this unusual pattern originates from an interaction between El Nino and the seasonal evolution of temperatures in the western tropical Pacific warm pool.

“Not all El Nino events are accompanied by this unusual wind pattern,” Stuecker said, “but once El Nino conditions reach a certain threshold amplitude during the right time of the year, it is like a jack-in-the-box whose lid jumps open.”

A study of the evolution of the anomalous wind pattern in the model reveals a rhythm of about 15 months accompanying strong El Nino events, which is considerably faster than the three-to-five-year timetable for El Nino events, but slower than the annual cycle.

“This type of variability is known in physics as a combination tone,” said Fei-Fei Jin, Professor of Meteorology and co-author of the study.

Combination tones have been known for more than three centuries. They were discovered by violin builder Tartini, who realized that our ear can create a third tone, even though only two tones are played on a violin.

“The unusual wind pattern straddling the equator during an El Nino is such a combination tone between El Nino events and the seasonal march of the sun across the equator,” said co-author Axel Timmermann, climate scientist at the International Pacific Research Center and professor at the UH Manoa Department of Oceanography.

He added, “It turns out that many climate models have difficulties creating the correct combination tone, which is likely to impact their ability to simulate and predict El Nino events and their global impacts.”

The scientists are convinced that a better representation of the 15-month tropical Pacific wind pattern in climate models will improve El Nino forecasts.

Moreover, they say the latest climate model projections suggest that El Nino events will be accompanied more often by this combination tone wind pattern, which will also change the characteristics of future El Nino rainfall patterns.