Construct · 1 fields · 2 citations
One name. One construct. A landmark on the map.
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A squall is a sudden, sustained increase in wind speed (conventionally a jump of a defined magnitude lasting at least a minute or two, which distinguishes it from a brief gust), typically accompanying showers, thunderstorms, or a frontal passage. The term extends to the squall line, a long organised band of thunderstorms along or ahead of a cold front; Newton's 1950 Structure and mechanism of the prefrontal squall line described the airflow and lifting that organise such a line, and Wallace and Hobbs's Atmospheric science places squalls among convective wind phenomena. The referent is a short-lived but sustained wind surge, and the convective line it names.[1][2]
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