2015
DOI: 10.1364/oe.23.033335
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Computationally efficient autoregressive method for generating phase screens with frozen flow and turbulence in optical simulations

Abstract: We present a sample-based, autoregressive (AR) method for the generation and time evolution of atmospheric phase screens that is computationally efficient and uses a single parameter per Fourier mode to vary the power contained in the frozen flow and stochastic components. We address limitations of Fourier-based methods such as screen periodicity and low spatial frequency power content. Comparisons of adaptive optics (AO) simulator performance when fed AR phase screens and translating phase screens reveal sign… Show more

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Cited by 22 publications
(8 citation statements)
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“…We do not consider the effects of residual uncorrected aberrations (i.e., the phase screen PSD amplitude and shape should be significantly larger, on the order of tens of microns rms, and closer to -11/3, respectively, beyond the spatial frequencies corresponding to the DM control radius) and therefore will not analyze performance beyond the 16 λ/D control radius. We use the framework from Srinath et al (2015), where the α parameter, a dimensionless number between 0 and 1, is used to simulate atmospheric "boiling," or deviating random effects from pure frozen flow; e.g., α = 0.95 means that 95% of the current phase screen (or 100 2 (0.95) ≈97 nm rms) will be translated to the next phase screen realization via a Fourier shift based on the time interval, telescope diameter, and wind speed and direction, whereas as the other 100 2 (1 − 0.95) ≈22 nm rms component of the next phase screen realization will be randomly generated, but with the same -2 power law. In this paper we use a windspeed of 10 m/s in the +x pupil direction, 1 ms time intervals, and α = 0.95 (i.e., 5% random turbulence is added every ms).…”
Section: A2 Post-processing Algorithmsmentioning
confidence: 99%
“…We do not consider the effects of residual uncorrected aberrations (i.e., the phase screen PSD amplitude and shape should be significantly larger, on the order of tens of microns rms, and closer to -11/3, respectively, beyond the spatial frequencies corresponding to the DM control radius) and therefore will not analyze performance beyond the 16 λ/D control radius. We use the framework from Srinath et al (2015), where the α parameter, a dimensionless number between 0 and 1, is used to simulate atmospheric "boiling," or deviating random effects from pure frozen flow; e.g., α = 0.95 means that 95% of the current phase screen (or 100 2 (0.95) ≈97 nm rms) will be translated to the next phase screen realization via a Fourier shift based on the time interval, telescope diameter, and wind speed and direction, whereas as the other 100 2 (1 − 0.95) ≈22 nm rms component of the next phase screen realization will be randomly generated, but with the same -2 power law. In this paper we use a windspeed of 10 m/s in the +x pupil direction, 1 ms time intervals, and α = 0.95 (i.e., 5% random turbulence is added every ms).…”
Section: A2 Post-processing Algorithmsmentioning
confidence: 99%
“…The atmospheric coherence length is a parameter of the simulation, which we use to adjust the average Strehl ratio of the PSF delivered by the AO correction. Our particular implementation of Kolmogorov turbulence employs the Fourier-based autoregressive algorithm of [26]; an example aberrated wavefront in the pupil plane generated with this method is shown in Fig. 3a.…”
Section: Wavefront Errormentioning
confidence: 99%
“…The most recent algorithms for generating atmospheric phase disturbance in simulation have been proposed to minimize computation time [21] as well as include the effects of boiling [22]. They also have flexible architectures that allow for the wind speed, outerscale and Fried parameter to vary at each time step.…”
Section: Simulating Atmospheric Phasementioning
confidence: 99%