2007
DOI: 10.1117/12.718257
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Comparing horizontal path C2n measurements over 0.6 km in the tropical littoral environment and in the desert

Abstract: We have measured the optical turbulence structure parameter, C 2 n , in two extremely different locations: the first being the littoral region on the southwest coast of Puerto Rico. The second location is over the dry desert in central New Mexico. In both cases, the horizontal beam paths are approximately 0.6 km long, within 2 meters of the local surface (Puerto Rico) and varying between 2 to 100 meters (New Mexico). We present our findings from the two datasets.

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Cited by 4 publications
(3 citation statements)
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“…Exact modelling of the turbulence is in fact ill-posed as it follows a non-uniform distribution which varies significantly in time, besides having an additional complexity introduced during the imaging process; thus, rendering the problem of modelling turbulence extremely difficult. Although the refraction index of the turbulent medium is often randomly changing, it is also statistically stationary [3], [30], [36]; thus, the deformations caused by turbulence are generally repetitive and locally centered [6], [7], [8], [9], [37]; this encourages the use of Gaussian-based models as approximate distributions that are general enough to avoid overfitting, but rather capture significant portion of the turbulent characteristics.…”
Section: Turbulence Modelmentioning
confidence: 99%
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“…Exact modelling of the turbulence is in fact ill-posed as it follows a non-uniform distribution which varies significantly in time, besides having an additional complexity introduced during the imaging process; thus, rendering the problem of modelling turbulence extremely difficult. Although the refraction index of the turbulent medium is often randomly changing, it is also statistically stationary [3], [30], [36]; thus, the deformations caused by turbulence are generally repetitive and locally centered [6], [7], [8], [9], [37]; this encourages the use of Gaussian-based models as approximate distributions that are general enough to avoid overfitting, but rather capture significant portion of the turbulent characteristics.…”
Section: Turbulence Modelmentioning
confidence: 99%
“…(x t w , y t h )) to model the turbulence motion in the scene. The locations visited by a particle moving due to the fluctuations of the turbulence have a unimodal and symmetric distribution which approaches a Gaussian [6], [30], [10], [9]. This is dissimilar from the linear motion of the particles driven by moving objects.…”
Section: Turbulence Modelmentioning
confidence: 99%
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