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Upper air flow, particularly in the form of divergent flow aloft, can strengthen a high-pressure system by promoting subsidence, which leads to clear skies and increased surface heating. As air descends, it warms and dries, enhancing the stability of the atmosphere. This process reduces cloud formation and precipitation, reinforcing the high-pressure system and allowing it to expand. Additionally, favorable upper-level winds can help maintain the high by reducing the likelihood of disturbances that might weaken it.

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1w ago

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