Fluctuations in backscattered signals due to turbulence in near-IR and visible lidar measurements

S. Fastig; Ariel Cohen

doi:10.1364/AO.27.001939

Fluctuations in backscattered signals due to turbulence in near-IR and visible lidar measurements

S. Fastig
, Ariel Cohen

Fredy & Nadine Herrmann Institute of Earth Sciences

Research output: Contribution to journal › Article › peer-review

2 Scopus citations

Abstract

Spectral cross-correlation measurements performed in the near IR and in the visible, λ1 = 1.06 μm and λ2 = 0.53 μm, show that the main contribution to the fluctuations for the above lidar wavelengths originate in atmospheric turbulence. The measurements were performed in nonsaturation conditions verified by an increase in the backscattered signal fluctuations with an increase in the target range. Normalized measurements as a function of daytime hours representing varying atmospheric turbulence conditions are presented and discussed.

Original language	English
Pages (from-to)	1939-1942
Number of pages	4
Journal	Applied Optics
Volume	27
Issue number	10
DOIs	https://doi.org/10.1364/AO.27.001939
State	Published - May 1988

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title = "Fluctuations in backscattered signals due to turbulence in near-IR and visible lidar measurements",

abstract = "Spectral cross-correlation measurements performed in the near IR and in the visible, λ1 = 1.06 μm and λ2 = 0.53 μm, show that the main contribution to the fluctuations for the above lidar wavelengths originate in atmospheric turbulence. The measurements were performed in nonsaturation conditions verified by an increase in the backscattered signal fluctuations with an increase in the target range. Normalized measurements as a function of daytime hours representing varying atmospheric turbulence conditions are presented and discussed.",

author = "S. Fastig and Ariel Cohen",

year = "1988",

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doi = "10.1364/AO.27.001939",

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N2 - Spectral cross-correlation measurements performed in the near IR and in the visible, λ1 = 1.06 μm and λ2 = 0.53 μm, show that the main contribution to the fluctuations for the above lidar wavelengths originate in atmospheric turbulence. The measurements were performed in nonsaturation conditions verified by an increase in the backscattered signal fluctuations with an increase in the target range. Normalized measurements as a function of daytime hours representing varying atmospheric turbulence conditions are presented and discussed.

AB - Spectral cross-correlation measurements performed in the near IR and in the visible, λ1 = 1.06 μm and λ2 = 0.53 μm, show that the main contribution to the fluctuations for the above lidar wavelengths originate in atmospheric turbulence. The measurements were performed in nonsaturation conditions verified by an increase in the backscattered signal fluctuations with an increase in the target range. Normalized measurements as a function of daytime hours representing varying atmospheric turbulence conditions are presented and discussed.

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Fluctuations in backscattered signals due to turbulence in near-IR and visible lidar measurements

Abstract

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