Retrieving "Warm Core Systems" from the archives

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1. Low Pressure Centers

   Linked via "warm-core systems"

   Tropical Cyclones
   These are warm-core systems fueled entirely by latent heat release from condensation over warm ocean waters (Sea Surface Temperature $> 26.5^\circ \text{C}$). They are characterized by a distinct central feature known as the eye (cyclone)/), a region of remarkably low pressure and sinking air. The [maximum sustained wind speed](/entries/…