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Air France jet may have hit a different kind of turbulence

Submitted by Blair Watson

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About: I am a freelance aviation journalist based in Kelowna, B.C. I have an airline transport pilot license with more than 4,000 hours of flying experience.

My take: I have one possible explanation for the disappearance of Air France Flight 447. It involves Clear Air Turbulence, something not mentioned in media reports on CBC. CAT, according to Wikipedia, is the "erratic movement of air masses in the absence of any visual cues, such as clouds. Clear air turbulence is caused when bodies of air moving at widely different speeds meet. At high altitudes (7,000-12,000 metres) this is frequently encountered around jet streams or sometimes near mountain ranges. Clear air turbulence is impossible to detect either with the naked eye or with conventional radar, meaning that it is difficult to avoid."

Did Air France Flight 447 encounter severe CAT? That is one of the questions that investigators will most likely consider if data eliminating that possibility is not discovered.

Peter Mansbridge on The National, on Monday, June 1, 2009, asked a guest pilot — how high can thunderstorms go — but the pilot did not answer. The answer is to heights greater than jetliner cruising altitudes, depending on the region, amount of heating of an air mass above a warm surface (land or water) and other factors.

Flying over southern Ontario on a hot, humid day, for example, I have heard pilots in jetliners at 41,000 feet ask air traffic control for permission to deviate from their course because the tops of thunderstorm cells were above their aircraft. In the tropical regions, such as the one where AF 447 was flying, thunderstorm clouds can reach even greater heights because the capping layer of the Earth's atmosphere, the tropopause, can reach 58,000 feet. that is well above jetliner cruising altitudes.

The amount of energy in a single, mature cumulonimbus (CB) thunderstorm cloud equals that of several Hiroshima-type atomic bombs. The speed of updrafts and downdrafts inside CBs can be several thousand feet per minute and the interface between them can tear aircraft apart. Additionally, pilots have tried to fly "saddleback," which means between vertical columns of convective cloud in thunderstorm areas, believing that the air "lane" ahead was clear, only to find themselves getting boxed in as the thunderstorm cells changed, which they always do.

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