Abstract
Aims. Current and future ground-based interferometers require knowledge of the atmospheric time constant t0, but this parameter has diverse definitions. Moreover, adequate techniques for monitoring t0 still have to be implemented. Methods. We derive a new formula for the structure function of the fringe phase (piston) in a long-baseline interferometer, and review available techniques for measuring the atmospheric time constant and the shortcomings. Results. It is shown that the standard adaptive-optics atmospheric time constant is sufficient for quantifying the piston coherence time, with only minor modifications. The residual error of a fast fringe tracker and the loss of fringe visibility in a finite exposure time are calculated in terms of the same parameter. A new method based on the fast variations of defocus is proposed. The formula for relating the defocus speed to the time constant is derived. Simulations of a 35-cm telescope demonstrate the feasibility of this new technique for site testing. © ESO 2006.
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Kellerer, A., & Tokovinin, A. (2007). Atmospheric coherence times in interferometry: Definition and measurement. Astronomy and Astrophysics, 461(2), 775–781. https://doi.org/10.1051/0004-6361:20065788
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