Source: wikibot/south-pacific-high

= South Pacific High
{wiki=South_Pacific_High}

The South Pacific High, also known as the South Pacific Anticyclone, is a large-scale high-pressure system that usually forms over the South Pacific Ocean, particularly during the Southern Hemisphere's summer months. It is characterized by relatively stable, dry atmospheric conditions and typically influences weather patterns over a significant portion of the South Pacific region. The South Pacific High plays a crucial role in the climate and weather of surrounding areas, including parts of Australia, New Zealand, and various islands in the Pacific.