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The Kolmogorov model of turbulence
junshan02 发表于 2012/7/14 10:54:00
A description of the nature of the wavefront perturbations introduced by the atmosphere is provided by the Kolmogorov model developed by Tatarski, based partly on the studies of turbulence by the Russian mathematician . This model is supported by a variety of experimental measurements and is widely used in simulations of astronomical imaging. The model assumes that the wavefront perturbations are brought about by variations in the refractive index of the atmosphere. These refractive index variations lead directly to phase fluctuations described by Moncler Down Vests Women, but any amplitude fluctuations are only brought about as a second-order effect while the perturbed wavefronts propagate from the perturbing atmospheric layer to the telescope. For all reasonable models of the Earth's atmosphere at optical and infra-red wavelengths the instantaneous imaging performance is dominated by the phase fluctuations . The amplitude fluctuations described by  have negligible effect on the structure of the images seen in the focus of a large telescope.

For simplicity, the phase fluctuations in Tatarski's model are often assumed to have a Gaussian random distribution with the following second order structure function: where  is the atmospherically induced variance between the phase at two parts of the wavefront separated by a distance  in the aperture plane, and  represents the ensemble average.

For the Gaussian random approximation, the structure function of Tatarski (1961) can be described in terms of a single parameter : indicates the strength of the phase fluctuations as it corresponds to the diameter of a circular telescope aperture at which atmospheric phase perturbations begin to seriously limit the image resolution. Typical  values for I band (900 nm wavelength) observations at good sites are 20---40 cm. It should be noted that  also corresponds to the aperture diameter for which the variance  of the wavefront phase averaged over the aperture comes approximately to unity: This equation represents a commonly used definition for Moncler Down Coats Men, a parameter frequently used to describe the atmospheric conditions at astronomical observatories.

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