2014
DOI: 10.1093/mnras/stu366
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Using the ${C_{n}^{2}}$ and wind profiler method with wide-field laser-guide-stars adaptive optics to quantify the frozen-flow decay

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Cited by 35 publications
(51 citation statements)
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“…Other sources have introduced a more sophisticated overlap factor (see e.g. Guesalaga et al 2014), but this is not necessary here, as we are not dealing with additional effects which can occur in real atmospheric images, such as shadows from mirror mounts or traces of laser guide stars. The approach to use a normalized cross-correlation in order to calculate an atmospheric shift is commonly used (Schöck & Spillar 2000;Wilson 2002;Guesalaga et al 2014).…”
Section: Wind Measurementmentioning
confidence: 99%
“…Other sources have introduced a more sophisticated overlap factor (see e.g. Guesalaga et al 2014), but this is not necessary here, as we are not dealing with additional effects which can occur in real atmospheric images, such as shadows from mirror mounts or traces of laser guide stars. The approach to use a normalized cross-correlation in order to calculate an atmospheric shift is commonly used (Schöck & Spillar 2000;Wilson 2002;Guesalaga et al 2014).…”
Section: Wind Measurementmentioning
confidence: 99%
“…As GeMS is a closed-loop system, the next step is to construct the pseudo-open-loop slopes (POLSs) from on-sky data using the actuator voltages, the interaction matrix and the residual slopes (see Cortés et al 2012 andGuesalaga et al 2014 for a detailed explanation). After subtracting tip and tilt, these slopes are used to construct the auto-correlation of slopes using the normalization of overlapping subapertures described in Butterley et al (2006) and Wang, Schöck & Chanan (2008).…”
Section: Estimating the Integrated Lmentioning
confidence: 99%
“…In fact, after eliminating the effect of noise in the telemetry data and using fitting techniques, two or more functions with different outer scale provide a much better representation. The sharper component could be caused by dome seeing (Guesalaga et al 2014) or ground turbulence (Dali et al 2010). This means that the use of a single L 0 is not adequate to describe the spatial coherence of the atmosphere, since the response function can be the result of combining slopes from more than one layer, each with different outer scale values, i.e.…”
Section: Estimating the Integrated Lmentioning
confidence: 99%
“…We implemented a system based on SLODAR method with ARGOS. The SLODAR technique must be modified to be applyed to AO system based on multiple laser guide stars and independent WFSs[4] [5]. The ARGOS's SLODAR is able estimate the turbulence strength in as many altitude bins as subapertures across the WFSs.…”
Section: Slodar Implementation With Argosmentioning
confidence: 99%