2002
DOI: 10.1117/12.460580
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Debunking the recurring myth of a magic wavelength for free-space optics

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Cited by 13 publications
(4 citation statements)
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“…Exact calculations and practical measurements (Ref. 2,3,4) indicate that longer wavelengths are less attenuated under light to moderate fog conditions, whereas under strong fog attenuation is equal for all wavelengths. There are even indications for a slight advantage of shorter wavelengths under extreme conditions.…”
Section: Availability Considerations For Fso Linkpath and Deploymentmentioning
confidence: 96%
“…Exact calculations and practical measurements (Ref. 2,3,4) indicate that longer wavelengths are less attenuated under light to moderate fog conditions, whereas under strong fog attenuation is equal for all wavelengths. There are even indications for a slight advantage of shorter wavelengths under extreme conditions.…”
Section: Availability Considerations For Fso Linkpath and Deploymentmentioning
confidence: 96%
“…The attenuation from dust and atmospheric aerosols are resulting from Mie scattering particles, which depend on the volume of the atmospheric aerosols, and the effects of absorption electromagnetic will be relatively small comparing with Mie scattering, therefore, the scattering coefficient can be computed form the visibility distance and wavelength of the incident beam. The range of visibility is related with concentration of dust as [5] :…”
mentioning
confidence: 99%
“…Thus, a strict radiation fog is a night time occurrence, although it may begin to form by evening twilight. Often it does not dissipate until after sunrise and has particle size distribution around 1-3 m [5]. Hence, it should affect more the short wavelength links and barely the 10 micron window.…”
Section: Theory and Experimentsmentioning
confidence: 97%
“…Radiation fog is the typical fog at that place. Advection fog, which is caused by the advection of moist air over a cold surface, cooling the air below the dew point, is known to display the largest particle size distribution [5] offering the worst conditions to 10 m light. Coastal upslope fog, which is formed when sea air flows upward over rising terrain and is adiabatically cooled to or below its dew point, also displays large particle size.…”
Section: Theory and Experimentsmentioning
confidence: 99%