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Actaully that is true with the U-2 - a 9 knot stall/ Vne window.Reminds me of a story that the P80 had a problem at 40000 feet in that the stall speed was almost as high as it's Mach number. A little slower and it stalled, a little faster and it was in compressibility.
Actaully that is true with the U-2 - a 9 knot stall/ Vne window.
The area most prone to failure was the tail - That came from Tony LeVier.A number of WW2 AC, when they got into compressibility, experienced the nose tucking under and attempting to correct using the elevators or trim tabs on the elevators usually was futile and could result in structural failure. The best means of dealing with compressibility and the resulting uncontrollable dive was to throttle back and wait for the airplane to get lower and into warmer air. Since the speed of sound varies only with air temperature, when the AC reached the warmer air it automatically came out of compressibility and became controllable. The problem with the P38 was that a number of them experienced structural failures during dives above 0.65 Mach.
Intuitively, not being an engineer, the tail section(s) of the P38 looks like where a failure would happen.
A number of WW2 AC, when they got into compressibility, experienced the nose tucking under and attempting to correct using the elevators or trim tabs on the elevators usually was futile and could result in structural failure. The best means of dealing with compressibility and the resulting uncontrollable dive was to throttle back and wait for the airplane to get lower and into warmer air. Since the speed of sound varies only with air temperature, when the AC reached the warmer air it automatically came out of compressibility and became controllable. The problem with the P38 was that a number of them experienced structural failures during dives above 0.65 Mach.
Bill, are you saying that the warmer the air the less dense it is and therefore the air plane has to go faster in warm air to encounter compressibility than it would in cold air? Was that not the reason the P38 encountered compressibility in the ETO more often than it did in the Pacific? The air was colder over Europe than over most of the Pacific. Would not the air at 30000 feet over Texas in August be warmer than the air over the Antarctic at 30000 feet in August?