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North Pacific high
[ nawrth puh-sif-ik hahy ]
noun
, Meteorology.
- a semipermanent subtropical high in the North Pacific Ocean, centered about 1,000 miles (1,600 kilometers) northeast of Hawaii, where it is strongest during the summer: As the North Pacific high becomes weakened and displaced toward the equator with the onset of winter, the Aleutian low becomes more dominant.
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Word History and Origins
Origin of North Pacific high1
First recorded in 1920–25
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