Poison:
Dear Ladies and Gentlemen,
The following information that is posted in this reply is something that may interest you all. The scenario was conducted several times and the results at the end of each scenario produced consistent findings.
In an A330 simulator at FL 350 with a gross weight of 210 tonnes in ISA+10, with icing selected, the aircraft approaches a thunderstorm with a high intensity of turbulence. Due to the extreme turbulence, the autopilot disengages. Shortly thereafter a malfunction is selected to block both captain and first officer's pitot tubes to replicate extreme ice formation.
The airplane reverts to alternate law with protection lost. There is a speed flag on both the captain and fo's PFD. The severe turbulence activates repeated stall warnings. Manual thrust is being used at this time. The speed on the standby altimeter is reading 240kts or thereabouts with MACH .72. From the GPS the ground speed is 350 kts or thereabouts. It is very difficult to read the instruments and ECAM warnings.
Updrafts take the aircraft up to FL 370 and produces a negative G of .2. The aircraft then enters severe downdrafts and the rate of descent averages more than 19,000 fpm. The instinctive reaction is to pull on the stick to arrest the rate of descent. The aircraft shakes and buffets violently. The G force on the SD reads +5 but the instructor's panel shows +8. The aircraft breaks up in flight around 20,000 ft.
After several attempts at this with all results being equal one could not see AF447 sending out any distress signals if this is what happened to them. Applying an unreliable airspeed memory item would have proven to be very difficult because of the violent shaking and opening a QRH for an ADR check procedure even less likely.
This could then explain why debris being located at present is both away from the flight plan, hard to locate, and now surfacing. The VS for example being in relatively good shape could have fluttered down like others have suggested. Considerable numbers if +5 or +8 g is reached.
