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  1. Atmospheric Pressure System

    Linked via "pressure gradient vector"

    The magnitude of the PGF ($\vec{F}_{PG}$) is mathematically defined as:
    $$ \vec{F}_{PG} = -\nabla P / \rho $$
    where $\nabla P$ is the pressure gradient vector and $\rho$ is the air density.
    The Coriolis Effect