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  1. Often called “popcorn” convection, single-cell thunderstorms are small, brief, weak storms that grow and die within an hour or so. They are typically driven by heating on a summer afternoon. Single-cell storms may produce brief heavy rain and lightning.

  2. Attenuation cells, (also known as Storm Cells, Soakaway Modules, and Storm Crates) are the modern equivalent of a soakaway. They allow surface water to be stored in one location and gradually released back to the ground, a bit at a time, at a pace the ground can handle, rather than in one sudden deluge, as happens during a storm or downpour.

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  3. en.wikipedia.org › wiki › Storm_cellStorm cell - Wikipedia

    A storm cell is an air mass that contains up and down drafts in convective loops and that moves and reacts as a single entity, functioning as the smallest unit of a storm-producing system.

  4. Jul 23, 1997 · With the two multicell storm categories, we have defined four basic storm types from the thunderstorm spectrum. The supercell is always severe, whereas the others can be non-severe or severe.

  5. The line of storms is often oriented north-south or northeast-southwest and generally move toward east while individual cells, comprising the line, move northeast. Like the multicellular cluster thunderstorms, new cells continually develop but this time on the leading, downwind, edge of the cluster.

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  6. Jan 6, 2024 · A supercell is a thunderstorm that rotates. There are three types of supercells: low-precipitation (LP), classic, and high-precipitation (HP). The configuration of the wind shear profiles within a severe weather environment is critical in diagnosing what types of supercells can be expected on a given day.

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  8. While each individual thunderstorm cell in a multi-cell cluster behaves as a single cell, the prevailing atmospheric conditions are such that as the first cell matures, it is carried downstream by the upper level winds, with a new cell forming upwind of the previous cell to take its place.

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