| Literature DB >> 23012524 |
Francisco J de Cos Juez1, Fernando Sánchez Lasheras, Nieves Roqueñí, James Osborn.
Abstract
In astronomy, the light emitted by an object travels through the vacuum of space and then the turbulent atmosphere before arriving at a ground based telescope. By passing through the atmosphere a series of turbulent layers modify the light's wave-front in such a way that Adaptive Optics reconstruction techniques are needed to improve the image quality. A novel reconstruction technique based in Artificial Neural Networks (ANN) is proposed. The network is designed to use the local tilts of the wave-front measured by a Shack Hartmann Wave-front Sensor (SHWFS) as inputs and estimate the turbulence in terms of Zernike coefficients. The ANN used is a Multi-Layer Perceptron (MLP) trained with simulated data with one turbulent layer changing in altitude. The reconstructor was tested using three different atmospheric profiles and compared with two existing reconstruction techniques: Least Squares type Matrix Vector Multiplication (LS) and Learn and Apply (L + A).Entities:
Keywords: MOAO; Zernike; adaptive; networks; neural; optics; reconstructor
Year: 2012 PMID: 23012524 PMCID: PMC3444082 DOI: 10.3390/s120708895
Source DB: PubMed Journal: Sensors (Basel) ISSN: 1424-8220 Impact factor: 3.576
Figure 1.Measurement of wave-front tilts.
Figure 2.Open loop adaptive optics.
Figure 3.Feedforward MLP neural network.
Summary of parameters of the neural network.
| Neural Network | Multi layer Perceptron |
| Number of hidden layers | 1 |
| Neurons | 222(input)-222(hidden)-27 (output) |
| Activation function | Continuous sigmoid function |
| Learning algorithm | Backpropagation error |
| Learning rate | 0.01 |
| Epochs | 10,000 |
Layer parameters of the three test cases.
| Common | Test name | test1 | test2 | test3 | |
| r0 | 0.16 | 0.12 | 0.085 | m | |
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| Layer 1 | Altitude | 0 | 0 | 0 | m |
| Relative strength | 0.65 | 0.45 | 0.8 | ||
| Wind Speed | 7.5 | 7.5 | 10 | m/s | |
| Wind direction | 0 | 0 | 0 | degrees | |
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| Layer 2 | Altitude | 4,000 | 2,500 | 6,500 | m |
| Relative strength | 0.15 | 0.15 | 0.05 | ||
| Wind Speed | 12.5 | 12.5 | 15 | m/s | |
| Wind direction | 330 | 330 | 330 | degrees | |
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| Layer 3 | Altitude | 10,000 | 4,000 | 10,000 | m |
| Relative strength | 0.1 | 0.3 | 0.1 | ||
| Wind Speed | 15 | 15 | 17,5 | m/s | |
| Wind direction | 135 | 135 | 135 | degrees | |
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| Layer 4 | Altitude | 15,500 | 13,500 | 15,500 | m |
| Relative strength | 0.1 | 0.1 | 0.05 | ||
| Wind Speed | 20 | 20 | 25 | m/s | |
| Wind direction | 240 | 240 | 240 | degrees | |
Network performance metrics with test 1, 2 and 3.
| Test 1 | RMSE | 0.8976 | 0.8464 | 0.6917 | 0.6159 | 0.6303 |
| Normalized Error | 0.0374 | 0.0345 | 0.1007 | 0.0844 | 0.0765 | |
| Accuracy | 94.8 | 97.13 | 77.22 | 80.1 | 83.63 | |
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| Test 2 | RMSE | 1.0445 | 1.0387 | 0.7746 | 0.6891 | 0.7121 |
| Normalized Error | 0.0314 | 0.0327 | 0.0773 | 0.0661 | 0.0614 | |
| Accuracy | 96.49 | 95.44 | 84.52 | 84.9 | 86.99 | |
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| Test 3 | RMSE | 1.0941 | 1.0902 | 1.0082 | 0.8701 | 0.9312 |
| Normalized Error | 0.0195 | 0.0200 | 0.0743 | 0.0589 | 0.0586 | |
| Accuracy | 99.29 | 99.46 | 85.94 | 85.91 | 89.7 | |
Test results with the three reconstruction techniques.
| Test 1 | Uncorrected | 644 | 0.048 |
| LS | 293 | 0.296 | |
| L + A | 251 | 0.402 | |
| ANN | 231 | 0.462 | |
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| Test 2 | Uncorrected | 817 | 0.025 |
| LS | 322 | 0.23 | |
| L + A | 289 | 0.3 | |
| ANN | 262 | 0.37 | |
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| Test 3 | Uncorrected | 1088 | 0.012 |
| LS | 454 | 0.068 | |
| L + A | 409 | 0.1 | |
| ANN | 387 | 0.125 | |
Wave-front Error and Strehl ratio for the three reconstruction at extreme test cases with increasing altitude.
| Uncorrected | 5,000 | 767 | 0.064 |
| LS | 293 | 0.289 | |
| L + A | 269 | 0.353 | |
| ANN | 211 | 0.52 | |
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| Uncorrected | 10,000 | 818 | 0.025 |
| LS | 465 | 0.066 | |
| L + A | 372 | 0.147 | |
| ANN | 297 | 0.287 | |
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| Uncorrected | 15,000 | 815 | 0.026 |
| LS | 574 | 0.043 | |
| L + A | 466 | 0.069 | |
| ANN | 390 | 0.127 | |
Figure 4.WFE as a function of turbulence strength r0 and the outer scale L0.
Figure 5.WFE as a function of turbulence strength r0 using Test 2 atmospheric profile.