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  2. Hook echo - Wikipedia

    en.wikipedia.org/wiki/Hook_echo

    A hook echo is a pendant or hook-shaped weather radar signature as part of some supercell thunderstorms. It is found in the lower portions of a storm as air and precipitation flow into a mesocyclone, resulting in a curved feature of reflectivity. The echo is produced by rain, hail, or debris being wrapped around the supercell. [1]

  3. Supercell - Wikipedia

    en.wikipedia.org/wiki/Supercell

    The first storm to be identified as the supercell type was the Wokingham storm over England, which was studied by Keith Browning and Frank Ludlam in 1962. [4] Browning did the initial work that was followed up by Lemon and Doswell to develop the modern conceptual model of the supercell. [ 5 ]

  4. Mesocyclone - Wikipedia

    en.wikipedia.org/wiki/Mesocyclone

    A mesocyclone is a meso-gamma mesoscale (or storm scale) region of rotation , typically around 2 to 6 mi (3.2 to 9.7 km) in diameter, most often noticed on radar within thunderstorms. In the Northern Hemisphere , it is usually located in the right rear flank (back edge with respect to direction of movement) of a supercell , or often on the ...

  5. Supercell thunderstorm moves across northwest after Greater ...

    www.aol.com/supercell-thunderstorm-moves-across...

    Around 100 properties were damaged by what police called a ‘localised tornado’ that whipped through Stalybridge, Tameside, on Wednesday.

  6. Bounded weak echo region - Wikipedia

    en.wikipedia.org/wiki/Bounded_weak_echo_region

    Vertical cross-section through a supercell showing the BWER. The bounded weak echo region, also known as a BWER or a vault, is a radar signature within a thunderstorm characterized by a local minimum in radar reflectivity at low levels which extends upward into, and is surrounded by higher reflectivities aloft, forming a kind of dome of weak echoes.

  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 ...

  8. What’s a supercell thunderstorm and the science behind the ...

    www.aol.com/news/supercell-thunderstorm-science...

    The near 26 inches of rain at Fort Lauderdale-Hollywood International Airport was a 1-in-1,000-year storm. Skip to main content. Sign in. Mail. 24/7 Help. For premium support please call: 800-290 ...

  9. English: A mature supercell thunderstorm over Needmore, Texas. May 4, 2019. May 4, 2019. This image shows the supercell updraft, downdraft, and a ragged lowering under the supercell's base.