How has El Niño affected your life?
El Niño Southern Oscillation (ENSO)
Oceans are able to store a lot of heat energy, but whereas the weather can change rapidly, it takes the ocean hundreds of years to warm up throughout its depths. Because the oceans can store heat, they slow down the rate of global warming and are therefore a major influence on the climate system. Individual oceans have their own circulation patterns; some of them region or local, and unusually cold or warm patches can persist for years. Some areas regularly oscillate between a warmer and a cooler state every few years. The best known of these is the El Niño Southern Oscillation (ENSO), in the eastern Equatorial Pacific, where the warm state is called El Niño and the cooler state is called La Niña. The El Niño straddles the equator; broad along the coasts of Ecuador and Peru, and getting narrower as it stretches west.
South America gave El Niño its name, calling it after the boy child (the Christ child) because it appears somewhere around Christmas. La Niña means the girl child. ENSO effects many weather systems, causing floods for some and droughts for others, in a pattern lasting 2 to 8 years. The severity of El Niños varies. There was a very large area of warm water for the El Niño which appeared in 1972, and it upset the pattern of rainfall around the world. Africa, Australia, India and the former Soviet Union suffered major droughts. The Mediterranean and the South American coast had heavy rainfall and extensive flooding.
The warm area can arise because the pattern of winds in the southwestern Pacific Ocean changes, allowing warm water to move to a different part of the ocean. During a strong El Niño event, the prevailing trade winds that blow from east to west across the equatorial Pacific weaken or blow in the opposite direction and the warmer surface water is forced eastwards. The warmer water means the atmosphere can pick up more moisture into the clouds, which is followed by heavier rain for parts of South America and less for others such as Indonesia. During La Niña the south east trade winds strengthen instead, pushing warmer water into the west Pacific, and causing more rain in the west and less in the east Pacific.
ENSO can also affect the pattern of monsoons, particularly where their peaks or troughs overlap (monsoons follow a different cycle). There were very strong ENSOs in 1877, 1884, 1891, 1899, 1911, 1918, 1925, 1941, 1957, 1972 and 1982. In 1877, 1899, 1918 and 1972 they coincided with monsoon phases and caused major droughts in Asia. 1997/98 was the second strongest El Niño in the past century; 2,000 people died. It was followed by a moderate La Niña.
Whilst the impact of El Niños is felt most strongly by the countries bordering the Pacific, in strong years the effects can spread further afield. for example a strong ENSO leads to a wetter than average spring in central Europe and southern England. This is because the atmospheric patterns over the Pacific can affect the strength and position of jet streams, which tend to be tracked by storms. Strong El Niños also cause more hurricanes and tropical storms to make landfall over the Gulf of Mexico and the Caribbean.
El Niño can also affect fish stocks and coral reefs (there was a record bleaching in 1997-1998 because of the elevated temperatures). El Niño droughts can lead to an increase in forest fires and loss of crops. El Niño rains can lead to extra soil erosion and destruction and loss of crops.
El Niños and La Niñas are known to have been happening for at least 15,000 years judging by archaeological evidence. Thanks to climate change, El Niño has been more frequent, intense and persistent since the 1970's. Climate modellers are unsure what will happen in the future, however. It could change rain and drought patterns, and could change the distribution of tropical cyclones, which get their energy from warm surface water.
ENSO is not the only oscillation; The North Atlantic Oscillation (NAO) is the next best known, affecting the westerly winds across western and northern Europe, affecting weather there and in the Mediterranean. The oscillations are not the only aspect of the climate that can flip-flop between states; another is the Ocean Conveyor Belt.
Forecasts Help Farmers Improve Harvest
Better access to and improvements to weather forecasting are helping farmers in Zimbabwe plan better and achieve higher harvests in what turned out to be better seasons. The El Nino weather phenomenon causes variation in the weather, so farmers not aware of what it is doing tend to either gamble and risk losing crops or hedge their bets.
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