ENSO: O MENINO QUE AQUECE O MAR NO NATAL

Published: 17 September 2024| Version 1 | DOI: 10.17632/vmggyrfpr6.1
Contributor:
Capitã Cintia Cardoso Capitã Cintia Cardoso

Description

El Niño is a climate phenomenon that occurs when the waters of the Equatorial Pacific Ocean warm abnormally. During El Niño, initially warm waters accumulate in the central and eastern Pacific region, with the change in the direction of the trade wind, they move from west (W) to east (E), influenced by the counter-trade winds. . Excess heat released into the atmosphere changes weather patterns around the world, which can cause intense rainfall, prolonged droughts, storms and hurricanes. As warmed ocean waters release energy (heat) into the atmosphere, global temperatures rise and affect all biodiversity. El Niño is part of a natural cycle called the El Niño- Southern Oscillation (ENSO), which alternates with periods of cooler La Niña waters on an irregular schedule. It has a significant impact on fisheries, affecting fish availability and the livelihoods of coastal communities

Files

Categories

Biological Oceanography, Marine Biodiversity, Marine Ecology, Ocean

Licence