Physicists and mathematicians of the Ural Federal University (UrFU) have calculated how external factors affect the behavior of El Niño – atmospheric and oceanic processes in the Pacific region. In the mathematical model, they accounted for wind, humidity, temperature, ocean currents, and other parameters that can lead to unpredictable El Niño results. This is a phenomenon in which the temperature of the upper Pacific Ocean rises and the near-surface waters shift eastward. The onset of El Niño affects rainfall, fisheries in Peru, Chile, Ecuador, and climate change on the planet. Description of the features of the unusual phenomenon and its scenarios, the scientists published in the journal Physica D: Nonlinear Phenomena.
“Our calculations have shown that the higher the intensity of the noise, the more unpredictable the consequences, the stronger the disturbances, the more intense El Niño will manifest itself. And for the system to get out of equilibrium, sometimes you need a little push: a change in humidity or ocean currents,” says Head of the Laboratory of multiscale mathematical modeling at UrFU Dmitri Alexandrov. “The mathematical model allowed us to show how the process will develop under the influence of one or another factor. That is, we did not predict when El Niño would appear or what its consequences for the global climate would be, we calculated possible scenarios of this phenomenon and showed that under some conditions there would be one version of events and under a different set of parameters there would be another.”
According to the calculations of physicists, external factors have a major impact on this phenomenon. For example, the stronger the wind, the greater the temperature amplitude. This, among other things, can throw the system out of balance and cause unpredictable weather phenomena.
“We based on the classical Vallis model, that describes El Niño. It is a simple model. It takes into account the temperature difference between the east and west coasts, the heat exchange between the Pacific Ocean and the atmosphere, and the velocity of air masses. We also took into account external noise – parameters that also affect atmospheric and oceanic processes. For example, changes in pressure, humidity, wind gusts, ocean currents,” says researcher.
These calculations may come in handy the next time El Niño appears. On the one hand, scientists still cannot predict when El Niño will come next, but, on the other hand, they have learned to predict how El Niño will behave. This is important because El Niño affects the climate as much as global climate change affects this phenomenon.
And if previously it was thought that the consequences of El Niño are observed only in South America, today scientists are confident that the abnormally warm water surface affects the weather of most of the Pacific Ocean, up to the 180th meridian. At the same time at El Niño periods global weather changes are more pronounced: large-scale changes in ocean temperature, precipitation, atmospheric circulation and vertical air movement over the tropical Pacific Ocean.
The essence of the process is this: there is a continuous warm current that originates off the coast of Peru and extends to the archipelago southeast of the Asian continent. It is an elongated region of heated water, about the size of the United States. Heated water vaporizes intensively and releases energy into the atmosphere. Clouds form over the heated ocean. Generally, trade winds (constant easterly winds in the tropical zone) move a layer of this warm water away from the U.S. coast toward Asia. Around Indonesia, the current stops, and monsoon rains fall on South Asia. During El Niño, the currents near the equator are warmer than usual, so the trade winds are weaker or not blowing at all. The heated water spreads out to the sides and flows back to the American coast. An anomalous zone of convection appears. Rains and hurricanes are hitting Central and South America.
“We believe that extreme El Niño events may become more frequent in the future and contribute to climate change, just as climate change affects El Niño development. Therefore, El Niño is a process that should be taken into account in global climate models, but this is not done yet, because no one knows how to take into account such an unpredictable and complex phenomenon,” add Dmitri Alexandrov.
El Niño is a natural phenomenon characterized by an abnormal increase in surface water temperature in the central and eastern equatorial zones of the Pacific Ocean. Usually on the Pacific coast of South America, ocean surface temperatures range from 59 – 66,2 ℉. During the El Niño period, the temperature rises by 35,6 – 50 ℉. During El Niño, the usual pattern of atmospheric processes in the tropical zone is disrupted, which can cause extreme climatic events around the world. The anomaly lasts from 8-9 months to a year or more.
Such fluctuations occur with periods from 2 to 10 years and exist (according to geological and paleoclimatic studies) for at least 300 thousand years. There have been several active El Niño cycles in recent decades: 1957-58, 1965-66, 1972-73, 1982-83, 1986-87, 1991-1993, 1994-95, 1997-98, and 2015-16.
Physica D Nonlinear Phenomena
How random noise induces large-amplitude oscillations in an El Niño model
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