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The pressure gradient decreases. drought conditions in Australia
During El Nino, the waters in the central and eastern tropical Pacific Ocean become warmer than usual, leading to changes in weather patterns worldwide. This warming disrupts normal ocean and atmospheric circulation patterns, impacting weather systems.
During an El Nino event, the weakened trade winds allow warm surface waters in the western Pacific Ocean to move eastward towards South America. This can cause an increase in sea surface temperatures, changes in weather patterns, and disruptions in marine ecosystems.
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The difference between El Nino and La Nina is basically water temperatures. El Nino is warming surface water temperatures resulting in nutrient poor waters in the Equatorial Current while during La Nina, the water temperatures will be lower.
The pressure gradient decreases. drought conditions in Australia
El Nino waters are less dense because the waters are warmer and warm water is less dense than cool water. Also, it constantly rains over the ocean during the El Nino, and rain water is less dense than ocean water.
During El Nino, the waters in the central and eastern tropical Pacific Ocean become warmer than usual, leading to changes in weather patterns worldwide. This warming disrupts normal ocean and atmospheric circulation patterns, impacting weather systems.
During an El Nino event, the weakened trade winds allow warm surface waters in the western Pacific Ocean to move eastward towards South America. This can cause an increase in sea surface temperatures, changes in weather patterns, and disruptions in marine ecosystems.
earth guakes
Warmer than usual waters that can sometimes reach the southern California coast.
Cause it want to..
El Nino
El Nino
El Nino
The difference between El Nino and La Nina is basically water temperatures. El Nino is warming surface water temperatures resulting in nutrient poor waters in the Equatorial Current while during La Nina, the water temperatures will be lower.
During an El Nino event, the trade winds in the tropical Pacific weaken or even reverse direction. This weakening of the trade winds allows warm water to move eastward towards the coast of South America, disrupting normal oceanic and atmospheric patterns and leading to the warming of sea surface temperatures in the eastern Pacific.