2014
DOI: 10.1016/j.optcom.2014.05.039
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Temporal spectrum of atmospheric scintillation and the effects of aperture averaging and time averaging

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Cited by 33 publications
(33 citation statements)
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“…the regular motion of air cells due to thermal turbulence fluctuation can be determined. More variations of the refractive index results in random optical beam fluctuations at a frequency range of ∼10 Hz to about 800 Hz, typically for the PSD of scintillation for horizontal propagation path with a point Rx [9][10][11]27]. The optical beam interaction with the atmosphere along the optical path is not the same throughout due to the random fluctuations and power loss of the air mass along the FSO path.…”
Section: Fso Communication Channels: Atmospheric Space and Underwatermentioning
confidence: 99%
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“…the regular motion of air cells due to thermal turbulence fluctuation can be determined. More variations of the refractive index results in random optical beam fluctuations at a frequency range of ∼10 Hz to about 800 Hz, typically for the PSD of scintillation for horizontal propagation path with a point Rx [9][10][11]27]. The optical beam interaction with the atmosphere along the optical path is not the same throughout due to the random fluctuations and power loss of the air mass along the FSO path.…”
Section: Fso Communication Channels: Atmospheric Space and Underwatermentioning
confidence: 99%
“…Since the atmospheric conditions play a vital role in determining the FSO system performance it needs to be accounted for while calculating the LM for any FSO system design. Existing LM models that include atmospheric channel and transmit-receive station parameters can be found in [9,10,15,27,31,32]. These models support the designers to have an optimum transmit-receive station parameter to initiate a data link with the maximum possible data rate for all weather conditions at a given location.…”
Section: Fso Communication Channels: Atmospheric Space and Underwatermentioning
confidence: 99%
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