Mindanao eddy: Difference between revisions
From Glossary of Meteorology
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<div class="definition"><div class="short_definition">A [[recirculation]] system between the [[North Equatorial Current]] and the [[North Equatorial Countercurrent]] in the extreme west of the Pacific Ocean, east of Mindanao.</div><br/> <div class="paragraph">The [[circulation]] is counterclockwise, about 800 km in diameter, and reaches to a depth of 250 m. Its western part forms the [[Mindanao Current]].</div><br/> </div> | <div class="definition"><div class="short_definition">A [[recirculation]] system between the [[North Equatorial Current]] and the [[North Equatorial Countercurrent|North Equatorial Countercurrent]] in the extreme west of the Pacific Ocean, east of Mindanao.</div><br/> <div class="paragraph">The [[circulation]] is counterclockwise, about 800 km in diameter, and reaches to a depth of 250 m. Its western part forms the [[Mindanao Current]].</div><br/> </div> | ||
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Latest revision as of 16:26, 25 April 2012
Mindanao Eddy
A recirculation system between the North Equatorial Current and the North Equatorial Countercurrent in the extreme west of the Pacific Ocean, east of Mindanao.
The circulation is counterclockwise, about 800 km in diameter, and reaches to a depth of 250 m. Its western part forms the Mindanao Current.
