Aggregate Terminal Velocity/Temperature Relations

Disdrometer Terminal velocity Cold front Winter storm Freezing rain Degree (music)
DOI: 10.1175/2008jamc1869.1 Publication Date: 2008-06-03T20:32:50Z
ABSTRACT
Abstract Terminal velocities of snow aggregates in storms along the Front Range eastern Colorado are examined with a ground-based two-dimensional video disdrometer. Power-law relationships for particles having equivalent volume diameters 0.5–20 mm computed temperatures −1°, −5°, and −10°C. Fall speeds increase temperature. Comparison found literature suggests that temperature-dependent relations may be surrogates based on aggregate composition (e.g., plates, columns, or dendrites) degree riming.
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