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  2. Pajama Sam 2: Thunder and Lightning Aren't so Frightening

    en.wikipedia.org/wiki/Pajama_Sam_2:_Thunder_and...

    While watching television, Sam gets startled by a thunderstorm and decides to make it stop by traveling to World Wide Weather, the company that produces the weather. By stowing away in a crate to be carried into World Wide Weather, Sam infiltrates the building and confronts the workers Thunder and Lightning only to realize that they are very friendly and that thunderstorms are beneficial for ...

  3. Training (meteorology) - Wikipedia

    en.wikipedia.org/wiki/Training_(meteorology)

    Showers and thunderstorms along thunderstorm trains usually develop in one area of stationary instability, and are advanced along a single path by prevailing winds. Additional showers and storms can also develop when the gust front from a storm collides with warmer air outside of the storm. The exact process repeats in the new storms until ...

  4. Thunderstorm - Wikipedia

    en.wikipedia.org/wiki/Thunderstorm

    A thunderstorm, also known as an electrical storm or a lightning storm, is a storm characterized by the presence of lightning [1] and its acoustic effect on the Earth's atmosphere, known as thunder. [2] Relatively weak thunderstorms are sometimes called thundershowers. [3] Thunderstorms occur in a type of cloud known as a cumulonimbus. [4]

  5. Thundersnow - Wikipedia

    en.wikipedia.org/wiki/Thundersnow

    Thundersnow, also known as a winter thunderstorm or a thundersnow storm, is a thunderstorm in which snow falls as the primary precipitation instead of rain. It is considered a rare phenomenon. [ 1 ] It typically falls in regions of strong upward motion within the cold sector of an extratropical cyclone .

  6. Heat burst - Wikipedia

    en.wikipedia.org/wiki/Heat_burst

    In meteorology, a heat burst is a rare atmospheric phenomenon characterized by a sudden, localized increase in air temperature near the Earth's surface. Heat bursts typically occur during night-time and are associated with decaying thunderstorms. [1]

  7. Rear flank downdraft - Wikipedia

    en.wikipedia.org/wiki/Rear_flank_downdraft

    The rear flank downdraft can arise owing to negative buoyancy, which can be generated by cold anomalies produced at the rear of the supercell thunderstorm by evaporative cooling of precipitation or hail melting, or injection of dry and cooler air in the cloud, and by vertical perturbation pressure gradients that can arise from vertical gradients of vertical vorticity, stagnation of ...

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