Back Kwasi-lineêre konvektiewe stelsels Afrikaans Línea de turbonada Spanish Pagiliin Estonian Haize-erauntsien lerro Basque خط تندوزه Persian Kuuropilvijono Finnish Grain (météorologie)#Ligne de grains ou grain en ligne French Cóch líne Irish Zivatarlánc Hungarian Linea di groppo Italian
A squall line, or more accurately a quasi-linear convective system (QLCS), is a line of thunderstorms, often forming along or ahead of a cold front. In the early 20th century, the term was used as a synonym for cold front (which often are accompanied by abrupt and gusty wind shifts). Linear thunderstorm structures often contain heavy precipitation, hail, frequent lightning, strong straight-line winds, and occasionally tornadoes or waterspouts. Particularly strong straight-line winds can occur where the linear structure forms into the shape of a bow echo. Tornadoes can occur along waves within a line echo wave pattern (LEWP), where mesoscale low-pressure areas are present. Some bow echoes can grow to become derechos as they move swiftly across a large area. On the back edge of the rainband associated with mature squall lines, a wake low can be present, on very rare occasions associated with a heat burst.