The North Pacific High, also known as the Pacific High or California High, is a semi-permanent high-pressure system located in the North Pacific Ocean. It typically forms during the summer months and can influence weather patterns across the western United States, particularly California, as well as areas in the North Pacific region. Key characteristics of the North Pacific High include: 1. **Formation**: It develops as a result of warm ocean waters and atmospheric conditions, creating a zone of high pressure over the ocean.
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