1. Thunderstorms/Lightning and Tornadoes Jeff Gawrych Met 10

3. Thunderstorms are generally classified into one of two groups: Air Mass Thunderstorms Air Mass Thunderstorms Mesoscale Convective Systems Mesoscale Convective Systems Thunderstorms   These are not-so-intense storms that are short-lived and localized.  These systems lead to the generation of numerous thunderstorms. numerous thunderstorms.

4. These thunderstorms form within a single air mass and are not tied to fronts or mid-latitude cyclones. Daily solar heating is primarily responsible for rising air motion, producing rising cumulus clouds. producing rising cumulus clouds. These storms may go through growing, mature and dissipation stage In just an hour or two In just an hour or two Often associated with summer storms. Air Mass Thunderstorms

5. Air mass thunderstorms are “self extinguishing” –  their natural evolution forces their dissipation An updraft is required to release the latent heat that drives the thunderstorms. In the later stages, rainfall will lead to air cooling and a downdraft. This largely kills the updraft and thus the thunderstorm

7. As the name suggests, these thunderstorms are part of a mesoscale system. The horizontal scale of up to a few hundred kilometers. The actual structure of an these storms can vary considerably. Severe Thunderstorms

8. As the name suggests, these thunderstorms are part of a mesoscale system. The horizontal scale of up to a few hundred kilometers. The actual structure of an these storms can vary considerably. Severe Thunderstorms –mesoscale convective complexes –squall line thunderstorms –supercell thunderstorms

9. Severe Thunderstorms

10. Change in wind with altitude important to formation: “Wind Shear”

11. Squall-line Thunderstorms

12. Characteristics Definition of Severe Thunderstorm: Severe Thunderstorms –Capable of producing large hail –Strong gusty surface winds –Flash floods –Tornadoes –¾ inch hail or –Surface wind gusts of 50 knots

13. Supercell Thunderstorms

14. Average # of days thunderstorms observed

15. Average number of days hail observed

16. Lightning and Thunder Lightning is the discharge of electricity that occurs within a thunderstorm. The extreme heating associated with lightning causes air to expand rapidly, and produces sound waves we recognize as thunder. If you want to estimate the distance of an approaching thunderstorm: –Count the number of seconds between a lightning strike and the sound of thunder strike and the sound of thunder –For every five seconds, the storm is 1 mile away

18. Normal charge separation in a mature thunderstorm  Charge separation not fully understood, but  rapid convection (vertical motion) is certainly important

19. Separation of Charge in Clouds One theory suggests that the separation of charge is due to collisions between ice particles. After exchanging charge, the heavier ice crystals settle toward the cloud base. ++ - -

20. Development of lightning stroke

21. Cloud to Ground Lightning Strike Positive charge is drawn up to the stepped leader. Usually through the highest conducting object. The return stroke can travel at 1  10 8 ms -1 (roughly 1/3 the speed of light.) This return stroke is visible to the human eye. There are commonly three or four strokes along a common path, which is why it is sometimes appears like the lightning flickers.

23. Why one shouldn’t shelter under a tree during a thunderstorm…

24. It is estimated that globally 5000 people are killed by lightning annually. At any given moment there are ~ 1000 thunderstorms occurring over the globe. Two thirds of all lightning strikes occur within the tropics. Most lightning strikes are NOT cloud to ground strikes (20%) - rather cloud to cloud strikes are most common. Aircraft are usually not damaged by lightning strikes. Lightning Facts

25. Tornadoes … … are also called twisters or cyclones. … are rapidly rotating winds that blow around a small area of intense low pressure. … come in many shapes, but mostly look like funnels or tubes. … often descend from large cumulonimbus clouds. A funnel cloud is a tornado that doesn’t hit the ground. A waterspout is a tornado-like storm that occurs over the ocean

26. Tornado Characteristics  Majority of tornadoes rotate counter-clockwise (cyclonic)  Most tornadoes only last a few minutes  Most tornadoes are ~ 100 – 600 m (300-2000 ft) in diameter

28. Fujita Tornado Damage Scale F0......Gale tornado...... winds of 40-70 mph Some damage to chimneys; branches broken off trees, pushes over shallow-rooted trees… Fl...... Moderate tornado.....winds of 73-112 mph Peels surface off roofs; mobile homes destroyed. F2......Significant tornado......winds of 113-157 mph Considerable damage. Roofs torn off frame houses- mobile homes demolished; boxcars pushed over; larger trees snapped or uprooted-, light object projected like missiles.

29. Fujita Tornado Damage Scale F3......Severe tornado......winds of 158-206 mph Roof and some wall torn off, well constructed houses, trains overturned; most trees in forest uprooted F4......Devastating tornado......winds of 207-260 mph Well-constructed houses leveled, structures with weak foundations blown some distance; cars thrown… F5......Incredible tornado......winds of 261-318 mph Strong frame houses lifted off foundations and carried considerable distances to disintegrate- automobile sized missiles fly in excess of 100 meters; trees debarked; steel reinforced concrete badly damaged.

30. Tornado Formation  Formed in association with  Formed in association with severe thunderstorms is important  Conditionally unstable atmosphere is important  Multiple tornadoes can come from a single storm (like a supercell storm) Example: May 4-5, 2003, during a 24 hour period, there were over 80 reported tornadoes.Example: May 4-5, 2003, during a 24 hour period, there were over 80 reported tornadoes.

32. Recipe for a tornado  Strong wind shear - Can enhance rotation - Caused mainly by jet stream  Warm moist air below dry colder air - Large instability - Large instability - Explosive growth due to latent heat release  Supercell storms good candidate for tornadoes (they already have rotation).

33. Tornado occurrence? Tornadoes possible everywhere in the world, but most are in the U.S. (tornado alley Texas – Nebraska 3/4 of the tornadoes occur from March to July, with the maximum in _____.  Jet stream is still a large influence Most often occur in the _______________ Least frequent ______________ May late afternoon (4-6pm) before sunrise

34. Tornado incidence by state 25 year total

35. Why is Tornado Alley the most likely place to get tornadoes? Perfect location for the mixing of air masses Warm, moist gulf air to the south Cold, dry to the north/northeast Rockies mountains to west/northwest  Downslope flow is cool and dry Right latitude for the polar jet stream

36. On Radar, the presence of a hook echo indicates a mesocyclone; a region in a thunderstorm very likely to spawn a tornado