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In order to assess the adequacy of the MARINI-MURRAY model in terms of the
envisaged conditions in charter item 1, the model is compared with
the results of a raytracing algorithm, which uses the quite complex
refractive index formula derived by [Owens (1967)]. The atmosphere for the
raytracing algorithm is modeled in the same way as it is done in the
derivation of the MARINI-MURRAY model, i.e. a lapse rate of
,
atmospheric form factors according to equations 9 and
10 and a tropospheric height of 10 km.
Figure 1 shows the results obtained for the original
MARINI-MURRAY model (equation 12), for the modified
MARINI-MURRAY model (equation 13) and a third mapping
function derived from the GARDNER mapping function [Gardner and Rowlett (1976] namely
![\begin{displaymath}
\Delta R = \frac{1}{g(\phi,H)} \left [f_{Gr}(\lambda)
\frac{...
...{\sin(\theta_w)+0.017}}}
+ \frac{g_3}{\sin(\theta_w)} \right ]
\end{displaymath}](img39.png) |
(16) |
with the coefficients
The term 0.017 in the last denominator is again an empirical adjustment to
optimise convergence at low elevation angles. The number appearing in
coefficient C is not yet deduced to physical constants. Here again the wet
component of the correction was taken out of the continued fraction
expansion to ensure a proper treatment of dispersion.
Figure 1:
Comparison of mapping functions with raytracing for various
wavelengths and water vapour partial pressures.
|
|
As expected the MARINI-MURRAY mapping function serves best at it's design
wavelength of
with an error of up to 1.5 cm at 10 degrees
elevation and a humidity of 80 %. Generally speaking the highest deviations
(up to 4.5 cm) from the raytracing results show up at wavelengths far apart
from
and high humidities.
The modified MARINI-MURRAY mapping function compensates partly the errors
incurred by the incorrect dispersion model. Here the maximum deviations are
of about 1.5 cm.
It is to note, that the modified GARDNER mapping function performs very well
with deviations smaller than 2mm if we restrict ourselves to elevations
larger than 20 degrees.
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