Fri., Apr. 25, 2014

Friday Apr. 25, 2014

There's no one in the classroom before the start of the 2 pm class and we had time for "Suena mi guitarra", "Carrousel Sin Fin", and "Somewhere Else" from Federico Aubele.

The Foucault Pendulum reports and probably the Atmospheric Stability worksheets should be graded by Monday.

The first video of the day will contain
1. Some additional footage of the Andover KS tornado. We saw the same tornado, in a much weaker state, in class on Wednesday. It was the tornado that was filmed as it tore through a parking lot and the one that caught up the people driving on an interstate highway and forced them to seek shelter under a bridge. When you see it on the video today I think you will realize that it is larger and stronger now. There's a good possibility that the people in the earlier videos wouldn't have survived their encounter with a tornado this intense.

2. Pictures of new and distant supercell thunderstorms and wall clouds.

3. A computer simulation of the growth and development of a supercell thunderstorm.

But first we need to learn a little bit about supercell thunderstorms.

Here is a relatively simple drawing showing some of the key features on a supercell thunderstorm (found on p. 163 in the ClassNotes). In a supercell the rotating updraft (shown in red above) is strong enough to penetrate a little way into the stratosphere. This produces the overshooting top or dome feature above. A wall cloud and a tornado are shown at the bottom of the mesocyclone. In an ordinary thunderstorm the updraft is unable to penetrate into the very stable air in the stratosphere and the upward moving air just flattens out and forms an anvil. The flanking line is a line of new cells trying to form alongside the supercell thunderstorm (similar to convergence between prexisting winds and thunderstorm downdraft winds that can lead to new storm development alongside a dissipating air mass thunderstorm).

Here is a second slightly more complicated and realistic drawing of a supercell thunderstorm. A typical air mass thunderstorm (purple) has been drawn in so that you can appreciated how much larger supercell thunderstorms can be.

And for the first time this semester I was able to get the VCR in the class room to work and a videotape segment was shown at this point. It showed a distant supercell thunderstorm and photographs of the bases of nearby supercell thunderstorms. Here you could see the spectacular wall cloud that often forms at the base of these storms. Finally a computer simulation showed some of the complex motions that form inside supercell thunderstorms, particularly the tilted rotating updraft. I haven't been able to find the video online (that's why it was so important that the VCR work).

Thunderstorms with rotating updrafts and supercell thunderstorms often have a distinctive radar signature called a hook echo.

In some ways a radar image of a thunderstorm is like an X-ray photograph of a human body.

An X-ray doesn't image all the parts of the body, often just the skeleton (it depends on the strength of the x-ray beam and the sensitivity of the detector). The same is true with radar. It doesn't "see" everything inside a cloud.

The radio signals emitted by radar pass through the cloud itself but are reflected by the much larger precipitation particles. The radar keeps track of how long it takes for the emitted signal to travel out to the cloud, be reflected, and return to the radar antenna. The radar can use this to determine the distance to the storm. It also knows the direction to the storm and can locate the storm on a map. The intensity of the reflected signal (the echo) is often color coded. Red means an intense reflected signal and heavy precipitation. The edge of the cloud isn't normally seen on the radar signal.

A Doppler radar (something we didn't discuss in class) can detects small shifts in the frequency of the reflected radar signal caused by precipitation moving toward or away from the radar antenna. This can be used to determine wind speeds inside the tornado.

Here is an actual radar image with a prominent hook echo. The hook is evidence of large scale rotation inside a thunderstorm and means the thunderstorm is capable of, and may already be, producing tornadoes.

This is the radar image of a thunderstorm that produced a very strong tornado that hit Oklahoma City in May 1999
( http://www.spc.noaa.gov/faq/tornado/radscel.htm ). The hook echo is visible near the lower left hand corner of the picture. Winds in the tornado may have exceeded 300 MPH. You can read more about this tornado here. And here is some storm chase video of the tornado.

The figure below (p. 162 in the ClassNotes) illustrates the life cycle of a tornado. Have a close look at the next tornado you see on video and see if you can determine whether it is in one of the early or late stages of its development.

Tornadoes begin in and descend from a thunderstorm. You would usually see a funnel cloud dropping from the base of the thunderstorm. Spinning winds will probably be present between the cloud and ground before the tornado cloud becomes visible. The spinning winds can stir up dust at ground level. The spinning winds might also be strong enough at this point to produce some minor damage. Here is video of the Laverne Oklahoma tornado that was shown in class and that shows the initial dust swirl stage very well.

In Stage 2, moist air moves horizontally toward the low pressure in the core of the tornado. This sideways moving air will expand and cool just as rising air does (see figure below). Once the air cools enough (to the dew point temperature) a cloud will form.

Tornadoes can go from Stage 2 to Stage 3 (this is what the strongest tornadoes do) or directly from stage 2 to stage 4 or 5. Note a strong tornado is usually vertical and thick as shown in Stage 3. "Wedge tornadoes" actually appear wider than they are tall.

The thunderstorm and the top of the tornado will move faster than the surface winds and the bottom of the tornado. This will tilt and stretch the tornado. The rope like appearance in Stage 5 is usually a sign of a weakening (though still a dangerous) tornado.

A tornado cloud forms is mostly the same way that ordinary clouds do. In an ordinary cloud (left figure above) rising air moves into lower pressure surroundings and expands. Expansion cools the air. If the air expands and cools enough (to the dew point) a cloud forms. In a tornado air moves horizontally into lower pressure at the core of the tornado. The air expands and cools just like rising air does. If the air cools enough a cloud appears.

It is very hard to actually measure the speed of the rotating winds in a tornado. Researchers usually survey the damage caused by the tornado and assign a Fujita Scale rating. The original scale, introduced in 1971 by Tetsuya (Ted) Fujita. A simplified, easy to remember version is shown below. A very basic and grossly oversimplified damage scale is included. This is simple enough that I can remember it and can use it to estimate tornado intensity when I see damage on the television news.

The original scale has been revised because the estimated wind speeds were probably too high. The newer scale is called the Enhanced Fujita Scale and became operational in 2007. Here's a simplfied version of the EF scale

Now EF2, EF3 and EF4 levels have winds between 100 and 200 MPH and only EF5 tornadoes have winds over 200 MPH. More accurate versions of both scales are compared below.

The original Fujita Scale actually goes up to F12 (an F12 tornado would have winds of about 740 MPH, the speed of sound). Roughly 3/4 of all tornadoes are EF0 or EF1 tornadoes and have winds that are less than 100 MPH. EF4 and EF5 tornadoes are rare but cause the majority of tornado deaths.

The EF scale considers 28 different "damage indicators," that is, types of structures or vegetation that could be damaged by a tornado. Examples include:

Damage Indicator	Description
2	1 or 2 family residential home
3	Mobile home (single wide)
10	Strip mall
13	Automobile showroom
22	Service station canopy
26	Free standing light pole
27	Tree (softwood)

Then for each indicator is a standardized list of "degrees of damage" that an investigator can look at to estimate the intensity of the tornado. For a 1 or 2 family home for example

degree of damage	description	approximate wind speed (MPH)
1	visible damage	65
2	loss of roof covering material	80
3	broken glass in doors & windows	95
4	lifting of roof deck, loss of more than 20% of roof material, collapse of chimney, garage doors collapse inward, destruction of porch roof or carport	100
5	house slides off foundation	120
6	large sections of roof removed, most walls still standing	120
7	exterior walls collapse (top story)	130
8	most interior walls collapse (top story)	150
9	most walls in bottom floor collapse except small interior rooms	150
10	total destruction of entire building	170

You'll find the entire set of damage indicators and lists of degrees of damage here.
Here's some recent video of damage being caused by a tornado as it happened (caught on surveillance video). The tornado struck West Liberty, Kentucky on March 2 this year.

EF2 Damage roof is gone, but all walls still standing	EF4 Damage only the strong reinforced concrete basement walls are left standing. It doesn't look like there would have been anywhere in this building that would have provided protection from a tornado this strong.	EF5 Damage complete destruction of the structure

Here are some additional, older, photographs of typical damage associated with all the levels on the Fujita Scale. None of these photos was shown in class.

And finally, something that was initially a puzzle.

Several levels of damage (EF1 to about EF3) are visible in the photograph above. It was puzzling initially how some homes could be nearly destroyed while a home nearby or in between was left with only light damage. One possible explanation is shown below.

Some big strong tornadoes may have smaller more intense "suction vortices" that spin around the center of the tornado (they would be hard to see because of all the dust in the tornado cloud. Tornado researchers have actually seen the pattern shown at right scratched into the ground by the multiple vortices in a strong tornado.

The sketch above shows a tornado located SW of a neighborhood. As the tornado sweeps through the neighborhood, the suction vortex will rotate around the core of the tornado.

The homes marked in red would be damaged severely. The others would receive less damage. Just one suction vortex was used here, there are usually several. But the tornado diameter is probably larger than shown here.

At this point we watched the last of the tornado video tapes. It showed a tornado that occurred in Pampa, Texas (here are a couple of videos that I found on YouTube: video 1, video 2, they're missing the commentary that was on the video shown in class). Near the end of the segment, video photography showed several vehicles (pick up trucks and a van) that had been lifted 100 feet or so off the ground and were being thrown around at 80 or 90 MPH by the tornado winds. Winds speeds of about 250 MPH were estimated from the video photography (though the wind speeds were measured above the ground and might not have extended all the way to the ground).