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No. El Nino usually produces low hurricane activity in the Atlantic by increasing wind shear, which intereferes with a hurricane's ability to organise.
High wind shear
El Nino produces wind shear over the tropical Atlantic in the region where storms off NW Africa try to mature into hurricanes
effect on the atlantic ocean
El Nino reduces the number of hurricanes in the Atlantic Basin primarily due to increased wind shear, which tends to tear the storms apart before they can really develop. In the Pacific, there is usually more activity, but it is focused further to the east in the Western Pacific, not moving west of Korea and Japan as much.
No. El Nino usually produces low hurricane activity in the Atlantic by increasing wind shear, which intereferes with a hurricane's ability to organise.
High wind shear
El Nino produces wind shear over the tropical Atlantic in the region where storms off NW Africa try to mature into hurricanes
effect on the atlantic ocean
El Nino reduces the number of hurricanes in the Atlantic Basin primarily due to increased wind shear, which tends to tear the storms apart before they can really develop. In the Pacific, there is usually more activity, but it is focused further to the east in the Western Pacific, not moving west of Korea and Japan as much.
The El Nino phase can cause an increase in number and intensity of hurricanes in the Atlantic Basin. It can cause severe floods in places such as southern California, and droughts in other locations.
The pressure gradient decreases. drought conditions in Australia
west wind drift or the humboldt current
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.
El Nino (~over the n)
El Nino brings increase precipitation to the eastern Pacific Ocean during the late winter. It also increases precipitation in the early spring in the Eastern Pacific.
The El Nino can not be prevented. The El Nino bounces from South America across the Pacific Ocean and then across the Indian ocean to Africa and then bounces back to South America. Another name for it is "The southern ocean oscillation."