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  1. Low Pressure Centers

    Linked via "International Meteorological Nomenclatural Society ($\text{IMNS}$)"

    Dynamic low-pressure systems arise from upper-atmospheric processes, primarily divergence aloft coinciding with convergence at the surface. The most significant examples are extratropical cyclones.
    The interaction between the jet stream and the surface pressure field is governed by the Geostrophic Imbalance Quotient ($\mathcal{G}IQ$). When the $…