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Continental Flight 3407: Weather in Buffalo & Aircraft Icing

Brian Neudorff @ 11:00 am February 13th, 2009 · 2 Comments


The investigation continues into what caused Continental Flight 3407 to crash into a house in Clarence Center, NY around 10:20 p.m. Thursday night. One of the possible causes that has been theorized is icing occurring on the planes wing.

At 10 p.m. the National Weather Service reported the following surface weather conditions. An air temperature of 33 F, winds were out of the west at 17 mph gusting to 25 mph. Light snow and a mist was reported with a visibility of 3 miles.

These weather conditions are not uncommon for Buffalo in the winter and although very strong and gusty winds impacted the region for most of the day Thursday, they had subsided 10 to 20 mph with just light snow & mist around the time of the crash. Around the time of the crash other pilots flying in and out of Buffalo were talking about rime ice forming on their planes and there being fog.
Image of Skew-T chart & upper-air sounding from AccuWeather.com

Ice could have occured

Anything at this point is just speculation but I came across a very informative article about what aircraft icing is from Aerospaceweb.org. They point out that, “icing is most common on smaller prop driven airplanes, such as commuters and general aviation aircraft.” Which appears to be what flight 3407 was, a Bombardier Q400, a twin-engine turboprop.

In the simplest of terms, icing can occur when air temperatures approach freezing this cools the metal surface of the plane to the same temperature. Then water droplets in the air or rain can freeze when it comes in contact with the surface of the plane. At times, liquid water can already be below freezing, we call this “Supercooled” water and this will also freeze immediately on contact with the plane’s surface.
How Icing Occurs
When this ice accumulates on the wing of a plane it changes the way air flows over and around the wing. This change has a negative effect on the aircraft performance.

Ice that collects on a lifting surface causes a reduction in the maximum lift and maximum angle of attack and an increase in drag. It is the reduction of the angle of attack that is usually the most significant problem. In the case of the wing, this reduction usually becomes a factor during an approach to land, when the angle of attack is increased, and the speed reduced. Due to the ice, what was previously a safe angle of attack is now a dangerous one, causing the wing to stall (lose lift) and nose down. During an approach, an airplane is usually close to the ground, which means a sudden loss of lift can have disastrous results.

All of this is speculation but temperatures were near freezing at the surface and below freezing the higher up you went. There was light snow and a wintry drizzle as the atmosphere was close to saturation, this is a very possible theory on what happen but there is still a lot to do before any of these questions are answered.

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Tags: Misc Weather · NY Weather · Weather News

2 responses so far ↓

  • 1 Civilsurfer // Sep 5, 2009 at 3:07 pm

    Does Accuweather fund upper-air observations now? On this blog you wrote “Actual Upper Air Measurements from AccuWeather.com” Please let me know if there are additional upper-air observations funded by accuweather? If not, please cite NWS as source for actual upper-air measurements.

  • 2 Brian Neudorff // Sep 6, 2009 at 9:55 am

    Civilsurfer – you are correct that AccuWeather does not fund actual Upper Air Measurements, That should and will now say “Actual Upper Air Chart Provided by AccuWeather.com” I am sorry to have offended you so much. That graph came from the AccuWeather.com site not the NWS site so I will give AccuWeather.com credit for the Skew-T image.

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