Late-January US snowstorm wasn't historically exceptional: NOAA
Despite its deadly impacts, the recent winter storm that battered much of the United States was not historically exceptional, official data showed Monday.
An ice storm is a mesoscale winter weather phenomenon characterized by prolonged freezing rain that accumulates as glaze ice on exposed surfaces, typically when a warm, moist air layer overrides a shallow subfreezing layer near the ground. Supercooled liquid droplets form in the warm layer, remain unfrozen while descending, and freeze on contact with surfaces at or below 0 °C, producing significant radial ice accretion. This process modifies surface roughness and load, impacting vegetation, infrastructure, and power systems, and alters surface energy and momentum fluxes. Ice storms are studied using synoptic analyses, vertical soundings, and microphysical models to understand boundary-layer thermodynamics and precipitation phase transitions.
Despite its deadly impacts, the recent winter storm that battered much of the United States was not historically exceptional, official data showed Monday.
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