Implications of four-dimensional weather cubes for improved cloud-free line-of-sight assessments of free-space optical communications link performance

Fiorino, Steven T.; Bose‐Pillai, Santasri R.; Schmidt, Jason D.; Elmore, Brannon J.; Keefer, Kevin

doi:10.1117/1.oe.59.8.081808

Cited by 1 publication

(1 citation statement)

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“…1 Fog severely affects free‐space optical communications technologies that use light propagation in the atmosphere to transmit data for telecommunications, computer networks, and even drone guidance. High‐energy laser (directed‐energy) defense systems have become popular because of their effectiveness in asymmetric warfare, for which optical scattering and molecular absorption and scattering from fog constitute a hindrance (Fiorino et al ., 2020; Kaymak et al ., 2018; Perram et al ., 2010). Knowledge of fog physics is also critical for better understanding of ecological processes, viticulture, and extraction of potable water from fog amidst global water crises and the looming threat of climate change (Klemm et al ., 2012; Weathers, 1999).…”

Section: Introductionmentioning

confidence: 99%

A mechanism for coastal fog genesis at evening transition

Hintz,

Huang,

Hoch

et al. 2024

Quart J Royal Meteoro Soc

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Transitional changes in the atmospheric boundary layer (ABL) are known to facilitate the onset of terrestrial fog, which is defined as a condition with near‐surface visibility <1 km due to airborne water droplets. In particular, the evening transition from a daytime convective ABL to a night‐time stable ABL provides favorable conditions for fog. This article describes a local fog event observed during the evening transition at a Canadian islet in the north Atlantic known as Sable Island during the “Fog and Turbulence Interactions in the Marine Atmosphere (Fatima)” field campaign. The comprehensive set of data collected using a myriad of instruments covering a wide range of scales allowed identification of a novel mechanism underlying this fog event. Therein an ocean–land discontinuity created a flow regime consisting of several stacked boundary layers, interplay of which produced a thin low‐level cloud that then diffused downward to the surface, causing visibility reduction. This mechanism offers useful insights on the role of boundary layers, stratification, and turbulence in fog genesis over oceanic islands.

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