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  2. Tornado debris signature - Wikipedia

    en.wikipedia.org/wiki/Tornado_debris_signature

    A tornadic debris signature (TDS), often colloquially referred to as a debris ball, [1] is an area of high reflectivity on weather radar caused by debris lofting into the air, usually associated with a tornado. [1] [2] A TDS may also be indicated by dual-polarization radar products, designated as a polarimetric tornado debris signature (PTDS).

  3. Hail spike - Wikipedia

    en.wikipedia.org/wiki/Hail_spike

    The multiple reflections of the radar beam causing the hail spike. Generally known as hail spikes, these are the result of energy from the radar hitting hail, very heavy rain, or in extreme cases, debris being lofted by a tornado, and being reflected to the ground, where they reflect back to the hail and then to the radar as in the image on the left. [1]

  4. Convective storm detection - Wikipedia

    en.wikipedia.org/wiki/Convective_storm_detection

    Nonmeteorological reflectors co-located with a couplet, can confirm that a tornado has likely occurred and lofted debris. An area of high reflectivity, or debris ball, may also be visible on the end of the hook. Either the polarimetric data or debris ball are formally known as the tornado debris signature (TDS).

  5. How to recognize a 'radar-confirmed tornado' - AOL

    www.aol.com/weather/recognize-radar-confirmed...

    When the rain starts to fall, people immediately look to the weather radar to see how long it will last. But when severe weather strikes, meteorologists can use this technology to pinpoint the ...

  6. Debris fallout - Wikipedia

    en.wikipedia.org/wiki/Debris_fallout

    The basic mechanism of debris fallout is debris lofted by a tornado's updraft winds high into the atmosphere. [4] Charles E. Anderson completed the first study focusing on debris fallout on the F5 1984 Barneveld tornado, which produced a large survey revealing a trail of paper debris as wide as 23 mi (37 km) at 110 mi (180 km) from Barneveld and a roughly 85 mi (137 km) long path of heavy ...

  7. MESO-SAILS - Wikipedia

    en.wikipedia.org/wiki/MESO-SAILS

    Multiple Elevation Scan Option for Supplemental Adaptive Intra-Volume Low-Level Scan [1] (abbreviated MESO-SAILS), [2] is a dynamic scanning option for the WSR-88D, controllable by the operator of the radar, when in VCP mode 12 and 212, and additionally 35 and 215 with the Build 18 update scheduled for October 2017. When active, anywhere from ...

  8. Cobra Dane - Wikipedia

    en.wikipedia.org/wiki/Cobra_Dane

    It is also listed as a partner of the NASA Orbital Debris Program Office and works with the Missile Defense Agency, [1] under the control of the 21st Operations Group. [7] The Cobra Dane radar has been upgraded to be integrated in the Missile Defense Agency's (MDA) Ballistic Missile Defense System (BMDS).

  9. Tornado vortex signature - Wikipedia

    en.wikipedia.org/wiki/Tornado_vortex_signature

    Strong mesocyclone on a thunderstorm near Tuscaloosa, Alabama, that was analyzed as fitting the characteristics of a TVS.It was associated with a tornado.. A tornadic vortex signature, abbreviated TVS, is a Pulse-Doppler radar weather radar detected rotation algorithm that indicates the likely presence of a strong mesocyclone that is in some stage of tornadogenesis. [1]