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what is causing the decline of havells india limited (517354) ✌️【Risk Management】✌️ Free global stock market data to help you plan the best investment strategies and seize market opportunities. Warm water normally is confined to the western Pacific by winds that blow from east to west, pushing it toward Indonesia and Australia. But during an El Niño, the winds slow down and can even reverse direction, allowing the warmer water to spread eastward all the way to South America.
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El Niños – among many large-scale weather patterns that act in tandem to influence global weather – occur every two to seven years in varying intensity, and the waters of the eastern Pacific can be up to 7 degrees Fahrenheit (4 degrees Celsius) warmer than usual.
El Niño, which in Spanish means “little boy,” is the opposite of the La Niña, or “little girl,” climate pattern.
It can especially affect thejet stream– a narrow band of strong wind in the upper atmosphere – over the Pacific, which gets stronger and dumps more frequent and intense storms over the western US, especially California, and along South America’s west coast.
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El Niño has been known to cause intense flooding across eastern sections of Africa – leading to landslides, an increase in waterborne diseases and even food shortages – while northern and southern parts of the continent experience severe drought.
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Like snowflakes, no two El Niños are exactly alike. For instance, an area of warmer water in the northern Pacific that became known as“the blob”during the 2014-2016 El Niño event wasn’t there during the 1997 El Niño.
But during typical El Niño years, more rain falls in the southwestern and southeastern United States, while the North experiences much drier and warmer weather.
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Climate change could make El Niños’ impact worse, somerecent studiesshow. And while the overall number of El Niños is unlikely to increase as the planet warms, amplified, so-called “super” El Niños will be twice as likely,other research suggests.
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