How Tornadoes Are Predicted
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How Tornadoes Are Predicted

How tornadoes are predicted days or hours in advance is not easy. There are numerous ingredients that cause tornadoes and go into predicting the possibility for tornadoes.

How tornadoes are predicted days or even hours in advance is not easy. There are numerous ingredients that cause tornadoes and go into predicting the possibility for tornadoes.

Predicting Tornadoes Days and Hours in Advance

Located in the middle of tornado alley in Norman, Oklahoma, the National Weather Service Storm Prediction Center (SPC) is the place that watches for the possibility of tornadoes and severe thunderstorms for the entire United States.

What is actually predicted days in advance is the likelihood or percentage possibility of tornadoes occurring in a certain area. The possibility of tornadoes can be predicted by watching for certain weather conditions with a fairly accurate percentage rate. The first ingredient forecasters could look at is warm humid air ahead of a predicted cold front, which can cause wind shear and is one ingredient in the formation of tornadoes. The cooler dry air behind a front meeting the warm humid air sometimes forms what is called a dryline, and at this juncture is where severe thunderstorms and tornadoes can form.

The National Weather Service (NWS) forecasters look at temperature, dew point and wind shear to determine the chances for severe thunderstorms that might produce a tornado in a given area. Wind shear is the changing of wind speed and or wind direction at different heights, from the surface upwards and is one main reason tornadoes form.

More Tornado Ingredients, CAPE and CIN

The NWS also look at something called CAPE, which stands for Convective Available Potential Energy of the atmosphere. CAPE is measured in joules per kilogram (j/kg) of energy. The higher the number, the more unstable the atmosphere is and the greater the chance of severe or tornado producing thunderstorms. CAPE measures the buoyancy of the atmosphere, the stronger the CAPE, the more upward force. Upward forcing is what causes updrafts, causing thunderstorms to grow taller, larger and more severe, which could lead to tornadoes.

A CAPE above 1200 j/kg is very unstable and could mean severe thunderstorms. But a high CAPE doesn’t always mean there will certainly be a severe thunderstorm or tornado, there are other factors as well.

CIN or the cap is another important factor whether or not a severe thunderstorm and tornadoes can form. CIN stands for convective inhibition. This means that the atmosphere is such that it inhibits updrafts, which means thunderstorms cannot form and if they do, they will not become severe or form tornadoes. CIN is like a cap or lid, capping the updrafts. If the cap is broken during the day, that is when a thunderstorm can rapidly develop and you can actually watch the updraft as the thunderstorm grows taller and could possibly become a severe thunderstorm and produce tornadoes.

The cap can usually be broken when the air temperature and the dew point reach a certain level. Knowing the CAPE, CIN, wind shear, temperature and dew point is a way to predict the possibility of severe thunderstorms and tornadoes for that day.

You can find out what your local NWS office predicts the CAPE to be for that day or days in advance by going to your local NWS web site and looking for what is called the “forecast discussion”. This is changed twice daily and is what the forecasters think is going to happen based on weather models, maps and atmospheric readings. At the end of the article, there is a link where you can get a 12-hour CAPE forecast map.

How Doppler Radar Can See Possible Tornadoes

NEXRAD, Next Generation Radar is a Doppler radar which can measure rainfall rates, intensity and wind speed and direction.

The radar beam returns a higher reading for intense rain and an even higher reading for hail since hail reflects a bigger signal back to the radar. Large hail is many times associated with severe thunderstorms and possible tornadoes.

When you look at NWS radar, you will see a graph that is labeled DBZ, which stands for decibels of reflectivity. This measures the intensity of the rain or hail in the thunderstorm. The larger the number, the more intense the storm is. Anything above 50 DBZ is considered a strong thunderstorm and could be capable of producing a tornado.

The Hook Echo

More importantly, Doppler radar can see motion. This can tell the meteorologist if a thunderstorm has a rotating column of air area within the thunderstorm called a mesocyclone. Approximately 40% of all mesocyclones produce tornadoes.

Meteorologists look at Doppler radar for signs that a severe thunderstorm is rotating which could produce a tornado. There is a certain signature on Doppler radar called a hook echo.

Rotation in a thunderstorm or mesocyclone can sometimes be seen on radar by what is called a hook echo. When the NWS sees a hook echo on their radar, many times they will then issue a tornado warning. What this hook echo actually is is rain wrapping around the rotation in that area of the thunderstorm. This rotation is in the thunderstorm, above the ground. Since this is not a ground level view by the radar, this doesn’t mean there is actual rotation on the ground like a tornado would cause, just that there is rotation in the storm and the rotation could form into a tornado.

1999 Oklahoma City tornado hook echo.                            Wind direction, notice where the winds change at the arrows.

Tornado Watches and Warnings

If the conditions look good that a certain area will have tornadoes, the Severe Prediction Center will issue a tornado watch. This means that there is a possibility of severe thunderstorms that can cause tornadoes in that area. This is the first step in predicting tornadoes.

A tornado warning is issued by the local NWS office when a tornado is already occurring or imminent. This means that the public or a trained weather spotter has seen a funnel or a tornado or meteorologist have seen a hook echo on radar.

Predicting Tornadoes with Computer Models

The SPC has collected data from hundreds of areas in the US that had tornado producing thunderstorms and put this data into an equation. This index is called the Significant Tornado Parameter and is now another tool in forecasting where and when severe thunderstorms and tornadoes might occur. New models are developed and tested each year to make predicting tornadoes more accurate.

Tornadoes cannot be predicted like a hurricane or even a day before they occur. But the NWS and the Severe Storm Prediction Center can give out good probabilities days and hours before. If you are interested in becoming a trained weather spotter, the article How to be a Storm Spotter will be of interest.

© 2010 Sam Montana

Resources 

Find your local NWS radar-Click on map of your location

12-hour CAPE map - click on CAPE/CIN

National Center for Atmospheric Research (NCAR)

NWS Storm Prediction Center

NOAA National Severe Storms Laboratory

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Comments (7)

Really interesting! Although sometimes the Pacific Northwest is dreary and gray for long periods of time, I'm grateful for its relative stability--the prospect of living through a tornado is really frightening. Thanks for your excellent explanation.

What the Pacific Northwest lacks in weather you make up with volcanoes, earthquakes and the occasional tsunami thrown in. Thunderstorms can pop up quickly, the other day I decided to take a quick nap after lunch and it was bright sunny out. 45 minutes later the tornado sirens startled me awake.

Facinating stuff Sam, fortunately here in The U.K, although we are always complaining about the weather, compared to some, we have nothing to gripe about.

Yeah--uh, Sam--I don't think my nervous system could survive that kind of ongoing threat. I would never nap again.

Great article ! We humans are still struggling to cope with nature and her fury....One Tsunami was enough to last for a life time ...

Very nice Darrell

I posted this to my facebook. I have friends in AZ who are dealing with tornadoes there.

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