On 02/13/2007 12:11 AM, Dave Perry wrote:

> .... I can see how you generate a table that gives PA and C(s) for
> layers with nonzero lapse rate.  I assume you use equation (8) solved
> for h to generate the table when lamda = 0.  

Yes, equation 8, but I don't even need to solve for h.

That's the funny thing about an interpolation table.  To
convert P(h) to h(P) all you need to do is transpose the
ordinate <--> abscissa on each line of the table.

> In this case, how do you
> account for S = 29.92 being different from Pb?  It seems to me that
> Equation (8) will give us neither PA nor the Kollsman correction.

I hope I never have to answer questions about that case.  I assume
that QNH values, considered as pressures, all lie at pressure
altitudes *well* within the troposphere.  So the Kollsman shift
term can be computed by reference to layer 0 using equation 6,
not 8.  (I believe that if this assumption is not valid, a
whole lot of things other than altimeters will be broken. :-)


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