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Entrainment Dynamics & Updraft Dilution: How Turbulent Mixing and Cloud Core Width Dictate Convective Storm Survival
WEATHER FORECASTING

Entrainment Dynamics & Updraft Dilution: How Turbulent Mixing and Cloud Core Width Dictate Convective Storm Survival

*On sweltering summer afternoons, thermodynamic charts promise explosive supercell thunderstorms, yet towering cumulus repeatedly stall and collapse. The culprit is entrainment—a violent, turbulent mixing process where cloud radius dictates life or death in the mid-troposphere.*

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Banner Cloud Dynamics & Aerodynamic Depressurization: How Leeward Airflow Separation and Dynamic Pressure Drops Sculpt Mountain Crest Plumes
WEATHER FORECASTING

Banner Cloud Dynamics & Aerodynamic Depressurization: How Leeward Airflow Separation and Dynamic Pressure Drops Sculpt Mountain Crest Plumes

Stand on the exposed granite crest of the Hörnli Ridge on the Matterhorn or gaze across the desolate glacial moraines beneath the East Face of Mount Fitz Roy, and mountain meteorology presents one of its most mesmerizing optical paradoxes. Overhead, the troposphere is an expanse of flawless, cloudless sapphire. Gale-force synoptic winds roar over the jagged summit arête from the west, buffeting the windward rock face without generating a wisp of vapor. Yet, directly attached to the leeward precipice—streaming rigidly into the void like a colossal, triangular silk pennant—hangs a dense, turbulent cloud.

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