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On Jun 18, 12:31*pm, bildan wrote:
This calculation must be done in the same domain and in the same units. *i.e. true airspeed + true rate of climb or indicated airspeed + indicated rate of climb in the air-data domain. *TE calculations can also be done entirely in the inertial domain though no such system exists to my knowledge. Don't mix units or domains. I think you've have hit the nail on the head. It's annoying that I missed that since I'd wondered some time ago about indicated vs. true rate of climb. The only remaining question in my mind is if IAS and IROC (Indicated ROC) change in the right manner. At 18k feet where the atmospheric density is roughly half that at sea level, TAS = SQRT(2) * IAS and "true kinetic energy" will be twice "indicated KE." For the two factors to cancel out, it would seem that the TROC (true ROC) would have to be twice the IROC, and that sounds right. But it would be nice if you could say a few words about why that's the case. Here's what I can see right now: If, as I seem to remember (and makes intuitive sense), pressure vs. altitude decays exponential, then the derivative of pressure versus altitude will be half what it was at sea level. If the vario measures the rate of change of pressure, then we'd get the factor of 2 we need and all would be well, but ... the capacity bottle has only half as many air molecules. If that has any impact on the vario (over and above the factor of 2 mentioned above), then it would seem like compensation would be altitude dependent. I suspect that it does not, but any words on why would be appreciated. Thanks. Martin |
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