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Class #9: Monday, July 19 Thunderstorms and tornadoes Chapter 14 1Class #9, Monday, July 19, 2010
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Fig. 14-CO, p. 370 2Class #9, Monday, July 19, 2010
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Fig. 14-1, p. 372 3Class #9, Monday, July 19, 2010
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Thunderstorms and Tornadoes Chapter 14 4Class #9, Monday, July 19, 2010
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Thunderstorms A storm containing lightening and thunder; convective storms Severe thunderstorms: one of large hail, wind gusts greater than or equal to 50kts, or tornado Ordinary Cell Thunderstorms – Air-mass thunderstorms: limited wind sheer – Stages: cumulus, mature, dissipating – Entrainment, downdraft, gust front 5Class #9, Monday, July 19, 2010
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Fig. 14-2, p. 373 7Class #9, Monday, July 19, 2010
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Fig. 14-2, p. 373 8Class #9, Monday, July 19, 2010
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Fig. 14-2, p. 373 9Class #9, Monday, July 19, 2010
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Fig. 14-4, p. 375 11Class #9, Monday, July 19, 2010
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Thunderstorms Multi-cell Thunderstorms Thunderstorms that contain a number of convection cells, each in a different stage of development, moderate to strong wind shear; tilt, over shooting top Gust Front: leading edge of the cold air out-flowing air; shelf cloud, roll cloud, outflow boundary Micro-bursts: localized downdraft that hits the ground and spreads horizontally in a radial burst of wind; wind shear, virga 12Class #9, Monday, July 19, 2010
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Fig. 14-6, p. 376 14Class #9, Monday, July 19, 2010
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Thunderstorms Multi-cell Thunderstorms – Squall-line thunderstorms; line of multi-cell thunderstorms, pre-frontal squall-line, derecho – Meso-scale Convective Complex: a number of individual multi-cell thunderstorms grow in size and organize into a large circular convective weather system; summer, 10,000km 2 18Class #9, Monday, July 19, 2010
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Fig. 14-10, p. 378 19Class #9, Monday, July 19, 2010
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Fig. 14-11, p. 378 20Class #9, Monday, July 19, 2010
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Stepped Art Fig. 14-11, p. 378 21Class #9, Monday, July 19, 2010
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Thunderstorms Supercell thunderstorms Large, long-lasting thunderstorm with a single rotating updraft Strong vertical wind shear Outflow never undercuts updraft Classic, high precipitation and low precipitation supercells Cap and convective instability Rain free base, low-level jet Surface, 850mb, 700mb, 500mb, 300mb conditions 28Class #9, Monday, July 19, 2010
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Fig. 14-23, p. 384 34Class #9, Monday, July 19, 2010
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Thunderstorms Thunderstorms and the Dryline Sharp, horizontal change in moisture Thunderstorms form just east of dryline cP, mT, cT Floods and Flash Floods Flash floods rise rapidly with little or no advance warning; many times caused by stalled or slow thunderstorm Large floods can be created by training of storm systems, Great Flood of 1993 35Class #9, Monday, July 19, 2010
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Fig. 1, p. 386 36Class #9, Monday, July 19, 2010
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Thunderstorms Topic: Big Thompson Canyon – July 31, 1976, 12 inches of rain in 4 hours created a flood associated with $35.5million in damage and 135 deaths Distribution of Thunderstorms – Most frequent Florida, Gulf Coast, Central Plains – Fewest Pacific coast and Interior valleys – Most frequent hail Central Plains 38Class #9, Monday, July 19, 2010
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Fig. 14-25, p. 387 39Class #9, Monday, July 19, 2010
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Thunderstorms Lightening and Thunder – Lightening: discharge of electricity in mature storms (within cloud, cloud to cloud, cloud to ground) – Thunder: explosive expansion of air due to heat from lightening – Electrification of Clouds: graupel and hailstones fall through supercooled water, ice crystals become negatively charged – Upper cloud positive, bottom cloud negative 42Class #9, Monday, July 19, 2010
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Fig. 2, p. 390 44Class #9, Monday, July 19, 2010
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Thunderstorms Observations: Elves – Blue jets, red sprite, ELVES The Lightening Stroke – Positive charge on ground, cloud to ground lightening – Stepped leader, ground stroke, forked lightening, ribbon lightening, bead lightening, corona discharge 47Class #9, Monday, July 19, 2010
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Thunderstorms Observation: Apple tree – DO NOT seek shelter during a thunderstorm under an isolated tree. Lightening Detection and Suppression – Lightening direction finder detects radiowaves produced by lightening, spherics – National Lightening Detection Network – Suppression: seed clouds with aluminum 49Class #9, Monday, July 19, 2010
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Fig. 14-32, p. 392 51Class #9, Monday, July 19, 2010
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Fig. 14-33, p. 393 52Class #9, Monday, July 19, 2010
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Fig. 14-34, p. 393 53Class #9, Monday, July 19, 2010
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Fig. 14-35, p. 394 54Class #9, Monday, July 19, 2010
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Fig. 14-36, p. 394 55Class #9, Monday, July 19, 2010
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Fig. 3, p. 395 56Class #9, Monday, July 19, 2010
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Fig. 14-37, p. 396 57Class #9, Monday, July 19, 2010
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Tornadoes Rapidly rotating column of air that blows around a small area of intense low pressure with a circulation that reaches the ground. Tornado life cycle – Organizing, mature, shrinking, decay stage Tornado outbreaks – Families, super outbreak 59Class #9, Monday, July 19, 2010
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Tornadoes Tornado Occurrence US experiences most tornadoes Tornado Alley (warm, humid surface; cold dry air aloft) Highest spring, lowest winter Tornado winds Measurement based upon damage after storm or Doppler radar For southwest approaching storms, winds strongest in the northeast of the storm, 220 kts maximum Multi-vortex tornados 60Class #9, Monday, July 19, 2010
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Tornadoes Seeking shelter – Basement or small, interior room on ground floor – Indoor vs. outdoor pressure The Fujita Scale – Based upon the damage created by a storm – F0 weakest, F5 strongest – Enhanced Fujita Scale 65Class #9, Monday, July 19, 2010
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Tornadic Formation Basic requirements are an intense thunderstorm, conditional instability, and strong vertical wind shear Supercell Tornadoes – Wind sheer causes spinning vortex tube that is pulled into thunderstorm by the updraft – Mesocyclone, BWER, rear flank downdraft, vertical stretching, funnel cloud, rotating cloud, wall cloud 66Class #9, Monday, July 19, 2010
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Table 14-1, p. 399 67Class #9, Monday, July 19, 2010
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Table 14-2, p. 400 68Class #9, Monday, July 19, 2010
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Table 14-3, p. 400 69Class #9, Monday, July 19, 2010
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Fig. 14-42, p. 400 70Class #9, Monday, July 19, 2010
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Fig. 14-43, p. 401 71Class #9, Monday, July 19, 2010
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Stepped Art Fig. 14-46, p. 402 75Class #9, Monday, July 19, 2010
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Tornadic Formation Nonsupercell Tornadoes – Gustnadoes – Land spout – Cold-air funnels 76Class #9, Monday, July 19, 2010
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Severe Weather and Doppler Radar Doppler radar measures the speed of precipitation toward and away radar unit Two Doppler radars can provide a 3D view TVS, Doppler lidar NEXRAD 79Class #9, Monday, July 19, 2010
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Fig. 14-49, p. 405 80Class #9, Monday, July 19, 2010
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Fig. 14-50, p. 405 81Class #9, Monday, July 19, 2010
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Fig. 14-51, p. 406 82Class #9, Monday, July 19, 2010
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Waterspouts Rotating column of air that is connected to a cumuliform cloud over a large body of water Tornadic waterspout 83Class #9, Monday, July 19, 2010
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Fig. 14-52, p. 409 84Class #9, Monday, July 19, 2010
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