The Science of Thunderstorms
All thunderstorms go through three stages: the cumulus stage, the
mature stage, and the dissipation stage. Depending on atmospheric
conditions, these three stages can take anywhere from 20 minutes to
several hours to occur.
There are four main types of thunderstorms: single cell, multicell,
squall line (also called multicell line) and supercell. Which type you
get depends on the instability and relative wind conditions in the
atmosphere’s different layers (called "wind shear"). Single cell storms
are the typical summer thunderstorm we experience in temperate locales.
They typically move, being a function of a local atmospheric
instability.
Multi cell storms can form clusters or “squall lines” (organized line of storms). They tend to form from convective updrafts in or near mountain ranges and linear weather boundaries, usually strong cold fronts or troughs of low pressure. Multicell line storms can span hundreds of miles. They move swiftly, and are preceded by a gust front. Heavy rain, hail, lightning, very strong winds and even isolated tornadoes can occur in a squall line.
Images @ Melonpopzdropz Flickr
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