Simultaneous daytime measurements of the atmospheric coherence diameter r(0) with three different methods.
The most common parameter used in characterizing atmospheric turbulence (seeing) is the atmospheric coherence diameter, or r(0). r(0) can be measured in many ways. Three such techniques that are useful when one is making daytime seeing measurements by observing the Sun are described. Results from an experiment in which r(0) was measured with all three methods are presented.
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Acton