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Lecture 13 (11/25)

Lecture 13 (11/25). Severe Storms. Severe Storm. A thunderstorm must have one or more of the following to be considered a severe storm: (NWS classification) Winds 58 mph (50 knots) or more Hail 3/4” in diameter or larger Tornado. Supercell Thunderstorms.

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Lecture 13 (11/25)

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  1. Lecture 13 (11/25) Severe Storms

  2. Severe Storm • A thunderstorm must have one or more of the following to be considered a severe storm: (NWS classification) • Winds 58 mph (50 knots) or more • Hail 3/4” in diameter or larger • Tornado

  3. Supercell Thunderstorms • A supercell thunderstorm is a t.s. with a deep rotating updraft (mesocyclone) • Updraft elements usually merge into the main rotating updraft and then accelerate rapidly • Flanking updrafts "feed" the supercell updraft, rather than compete with it • Small percentage of all t.s.’s are supercells but they cause the majority of damage

  4. Diagram of a Supercell

  5. A Look from the SE

  6. Types of Supercells • Low Precipitation - (LP) - high cloud bases, little precip, large hail and winds more likely than tornadoes, often form along dryline • High Precipitation - (HP) - occurs in very moist air, precipitation often wraps around wall cloud and tornado, hard to see except by Doppler radar, dangerous to chase (and easy to get dents in car with)

  7. Classic Supercell • Classic supercell - in between HP and LP • Most of precip is separated from updraft region • Good one to chase b/c you can usually see the wall cloud and tornado and stay out of it’s path

  8. Features of Supercells • Mesocyclone (p.125) organizes updraft and downdraft and keeps them separate • Updraft is slanted downwind (aloft) so hail/rain doesn’t fall through it and kill it • Supercell can last for hours and travel a hundred plus miles • Often moves to the right of the mean flow - has to do with rotation (vorticity) and propagation • What does propagation mean?

  9. How Supercells Move • Movement = Advection + Propagation • This little formula applies to pretty much everything in weather • advection = just the horizontal transport of the feature (like a supercell) along with the winds • propagation = development of the feature (usually happens towards inflow or flanking line in the case of a supercell)

  10. Overshooting Top • Overshooting top - characteristic of a strong updraft • The updraft goes higher than the rest of the clouds near it (in the anvil) • Overshoots the tropopause or equilibrium level btwn the troposphere & stratosphere • Updraft penetrates stratosphere and then is forced back down to equilibrium level

  11. Overshooting Top

  12. Mammatus • See bottom of p. 167 • Little puffy clouds extending downward from anvil • Indication of high turbulence and strong updraft(s) in vicinity • Remember, the harder and more defined cloud features are stronger than the soft and less defined features

  13. Mammatus pictures

  14. Pileus Clouds • Can form immediately above a growing updraft if it’s humid at upper levels • Don’t be fooled by the soft appearance of pileus - they can hide the hard features of the actual updraft • see p. 176 in text

  15. Pileus Picture

  16. Anvil • Strong winds at upper levels usually accompany supercell thunderstorms (they help the updraft tilt) • The winds push the anvil along with them at high speeds (>50 mph) • In a strong updraft, a small anvil will blow upstream too (called backsheared anvil) • Again, the harder the feature, the stronger the updraft

  17. Backsheared Anvil

  18. Wall Cloud • Wall cloud is a region of cloudiness beneath the rotating updraft region of a thunderstorm • Usually slopes toward the rain and hail shaft (bottom of wall cloud closer to precip than top) • Must be rotating for it to be classified as a wall cloud • Often confused with shelf clouds & scud

  19. Wall Cloud Picture

  20. Shelf Cloud • Usually slopes away from precipitation • Shelf cloud = feature of outflow whereas a wall cloud = feature of inflow

  21. Shelf Cloud

  22. Beaver’s Tail Beaver’s tail is just a flanking line of inflow winds

  23. Hail • Hail can be a very destructive force • Formation • Starts as frozen raindrop or groupel • Held aloft by thunderstorm’s updraft • Grow from riming or supercooled droplets freezing to hailstone

  24. Hail images

  25. More hail

  26. Lightning

  27. Tornadoes – Fujita scale • F0 Light damage. Wind up to 72 mph. • F1 Moderate damage. Wind 73 to 112 mph. • F2 Considerable damage. Wind 113 to 157 mph. • F3 Severe damage. Wind 158 to 206 mph. • F4 Devastating damage. Wind 207 to 260 mph. • F5 Incredible damage. Wind above 261 mph.

  28. Tracking Tornadoes

  29. For Next time • Homework is posted • No reading assignment

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