TL;DR: In this paper, the authors proposed a fast transmission relationship based on an exact Mie theory calculation valid in the 0.69- to 1.55-µm spectral bands.
Abstract: The principal disadvantage of using free space optics (FSO) telecommunication systems is the disturbing role played by the atmosphere on light propagation and thus on the channel capacity, availability, and link reliability. The wavelength choice is currently a subject of disagreement among designers and users of FSO equipments. Generally this equipment operates in the visible and the near IR at 690, 780, 850, and 1550 nm. Several authors affirm that equipment working at 1550 nm presents less atmospheric attenuation in the presence of fog and thus better link availability. Others consider that for dense fogs (visibility<500 m), all wavelengths are attenuated in the same way (wavelength independence). Fog attenuation in the visible and IR regions is reviewed from an empirical and theoretical point of view. Laser system performance in the presence of fog (advection and convection) in the 0.4- to 15-µm spectral zone is investigated using FASCOD computation. A transmission gain of 42% for a lasercom system working at 780 nm is observed compared to the same system working at 1550 nm. This gain reaches 48% if the same system works at 690 nm. Finally, we propose a fast transmission relationship based on an exact Mie theory calculation valid in the 0.69- to 1.55-µm spectral bands. It enables us to predict fog attenuation according to visibility without using heavy computer codes.
TL;DR: The fog that affected the Meuse Valley, Belgium, in December, 1930 led to the first scientific proof of the potential for atmospheric pollution to cause deaths and disease, and it clearly identified the most likely causes.
TL;DR: In this article, the average concentrations of combined amino compounds (CAC, e.g., proteins and peptides) were generally 4 to 5 times higher than those of free amino compounds.
TL;DR: In this paper, the authors reviewed the state of knowledge of atmospheric organic matter processing by fogs, with a focus on field observations, and discussed the occurrence of organic matter in fog, its solubility, characterization and molecular speciation.
TL;DR: In this paper, the extinction coefficient and the mean droplet terminal velocity in advection fog were analyzed using two PMS forward-scatter spectrometer probes (FSSP-100) at the AFGL Weather Test Facility at Otis Air National Guard Base, Massachusetts.
Abstract: Fog droplet spectra data were obtained in several advection fogs at the AFGL Weather Test Facility at Otis Air National Guard Base, Massachusetts, using two PMS forward-scatter spectrometer probes (FSSP-100). Approximately 90 h of droplet data were recorded simultaneously at 5 m and 30 m above the ground throughout the life cycle of 11 fogs during 1980 and 1981. This large data set was used to develop new parameterizations of the extinction coefficient and the mean droplet terminal velocity in terms of liquid water content and droplet concentration for fogs with liquid water contents greater than 0.018 g m−3. The advection fog data show an excellent correlation of 95% between the extinction coefficient and liquid water content. The regression line for these two quantities is more nearly linear than found by other investigators. The correlation between the mean droplet terminal velocity and various microphysical parameters is not as high as that for the extinction coefficient and liquid water cont...