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4. Applications to atmosphere models

We have performed a number of simulations using the 4-layers fit of Roggermann et al. (1995) to various models published in the literature, rescaling them for different values of tex2html_wrap_inline1069. Namely the Greenwood good seeing model (Greenwood 1977) is denoted by G-77; the fit with Maui (Hawaii) U.S. Air Force Optical Station (Miller et al. 1976) is denoted by SLC-N and the Hufnagel-Valley model (Hufnagel 1974) with an upper atmospheric wind of 54 miles per hour (tex2html_wrap_inline1071) is denoted by HV-54.

We have generated series of 65536 tilts for each of the four layers in a grid of 6 different tex2html_wrap_inline1073 values for each of the 3 different atmosphere models adopted. For each layer a normal distributed tilt with a dispersion given by (Sarazin & Roddier 1990):


equation308
has been calculated and propagated up to the mesospheric Sodium layer. The effective tilt height has been computed together with the residual jitter for each of the 65536 time-points taken into consideration.

  figure313
Figure 3: The histograms for tex2html_wrap_inline1075 and tex2html_wrap_inline1077 for D=8 m, tex2html_wrap_inline1081 m in the HV-54 model. The run is composed by 65536 realizations. As it can be seen tex2html_wrap_inline1083 follows roughly a Gaussian distribution, while the tex2html_wrap_inline1085 distribution is much more platicurtic

As it can be easily seen in Fig. 3 (click here) the distribution of the effective height is far from a Gaussian shape; however the final residual tilt tex2html_wrap_inline1087 distribution is very well fitted by a Gaussian distribution, so that it can be identified by the single figure of the dispersion tex2html_wrap_inline1089. Following Sandler et al. (1994) one can determine the Strehl ratio degradation contribution due only to the problem pointed out in this paper using the relationship:


equation321

The results of the simulation are collected in Tables 1 (click here) and 2 (click here) and in Fig. 4 (click here) for the cases of D = 3.58 m and D = 8.00 m telescopes; the fluctuations of the mean effective height tex2html_wrap_inline1095 are due to the different realizations of the same multi-layer models. In order to get a deeper insight on the meanings of the published numbers it is here recalled that the diffraction limit capabilities for a tex2html_wrap_inline1097 nm wavelengths, tex2html_wrap_inline1099 are respectively 33.9 mas and 15.2 mas for the two telescope aperture taken into consideration.

  table331
Table 1: The results for the perfomed simulation in the D=3.58 m case

  table343
Table 2: The same as for Table 1 (click here), in the D = 8.00 m telescope case

  figure355
Figure 4: Behaviour of SR vs. tex2html_wrap_inline1149 for D = 3.58 m (upper panel) and D = 8.00 m (lower panel) telescope


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