2022
DOI: 10.1364/ao.443698
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Characterizing turbulence profile layers through celestial single-source observations

Abstract: Future spacecraft missions aim to communicate with the Earth using near-infrared lasers. The possible bit rate of Free-Space Optical Communication (FSOC) is orders of magnitude greater when compared to current Radio Frequency (RF) transmissions. The challenge of groundspace FSOC is that atmospheric turbulence perturbs optical wavefront propagation. These wavefront aberrations can be measured using a Shack-Hartmann Wavefront Sensor (SHWFS). A ground-based Adaptive Optics (AO) system can mitigate these aberratio… Show more

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Cited by 7 publications
(5 citation statements)
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References 33 publications
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“…This reduction in scintillation is clearly observed as a reduction in power fades during the time that the pre-distortion AO system is on. A larger Fried parameter value of r0 = 9.2 cm (specified at 500 nm and at Zenith) was extracted from the WFS measurements for this link through a single-source observation technique, 21 thus quantifying the weaker turbulence conditions that were present.…”
Section: Resultsmentioning
confidence: 99%
“…This reduction in scintillation is clearly observed as a reduction in power fades during the time that the pre-distortion AO system is on. A larger Fried parameter value of r0 = 9.2 cm (specified at 500 nm and at Zenith) was extracted from the WFS measurements for this link through a single-source observation technique, 21 thus quantifying the weaker turbulence conditions that were present.…”
Section: Resultsmentioning
confidence: 99%
“…In pursuit of a comprehensive analysis, we have developed a MATLAB-based algorithm implementing the Learn & Apply (L&A) technique for tomographic reconstructions in LTAO systems. [1][2][6][7][8][9][10][11] Our primary objective is to assess the level of reconstruction errors encountered during the L&A algorithm's application.…”
Section: Introductionmentioning
confidence: 99%
“…The refractive index structure constant, C 2 n , has been used as an indicator to characterize and quantify the turbulent spatial fluctuations caused by temperature gradients [1,2], wherein n denotes the local refractive index of the atmosphere. Existing techniques for C 2 n measurements include scintillation detection and ranging (SCIDAR) [3], multiaperture scintillation sensor (MASS) [4,5], scintillator [6], Shack Hartmann wavefront sensor (SHWFS) [7][8][9][10][11][12][13], Differential Image Motion (DIM) Light Detection and Ranging (LIDAR) [14], acoustic meteorological radar (sodar) [15], and the balloon-borne microthermometry [16]. Indeed, various techniques exist for the measurement of C 2 n (h).…”
Section: Introductionmentioning
confidence: 99%