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20 October 2004Optical turbulence in the Antarctic atmosphere
Turbulence in the earth's atmosphere severely limits the resolution
and sensitivity of astronomical observations. The vertical
distribution of turbulence in the atmosphere has a profound effect on
the residuals after correction by an active instrument such as
adaptive optics or a fringe tracking interferometer. It has already
been shown that the South Pole has turbulence profiles unlike those
at any other site, dominated by ground layer turbulence, with low
free air seeing. This paper examines the meteorology, climatology and
atmospheric physics that produces these conditions. Combining meterological observations at remote sites with models of atmospheric turbulence allows quantitative extrapolation to the likely conditions at sites now under development and consideration that may provide the ultimate ground based site for near and mid-infrared interferometry. The high plateau sites in Antarctica will likely enable complete sky coverage for adaptive optics and interferometry in the near infrared with natural guide stars.
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James P. Lloyd, "Optical turbulence in the Antarctic atmosphere," Proc. SPIE 5491, New Frontiers in Stellar Interferometry, (20 October 2004); https://doi.org/10.1117/12.552226