Articles | Volume 21, issue 17
Atmos. Chem. Phys., 21, 13099–13117, 2021
Atmos. Chem. Phys., 21, 13099–13117, 2021

Research article 03 Sep 2021

Research article | 03 Sep 2021

A new conceptual model for adiabatic fog

Felipe Toledo et al.

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Subject: Clouds and Precipitation | Research Activity: Remote Sensing | Altitude Range: Troposphere | Science Focus: Physics (physical properties and processes)
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Cited articles

Albrecht, B. A., Fairall, C. W., Thomson, D. W., White, A. B., Snider, J. B., and Schubert, W. H.: Surface-based remote sensing of the observed and the Adiabatic liquid water content of stratocumulus clouds, Geophys. Res. Lett., 17, 89–92,, 1990. a, b, c
Bergot, T.: Small-scale structure of radiation fog: a large-eddy simulation study, Q. J. Roy. Meteor. Soc., 139, 1099–1112, 2013. a
Bergot, T.: Large-eddy simulation study of the dissipation of radiation fog, Q. J. Roy. Meteor. Soc., 142, 1029–1040, 2016. a
Betts, A. K.: Cloud Thermodynamic Models in Saturation Point Coordinates, J. Atmos. Sci., 39, 2182–2191,<2182:CTMISP>2.0.CO;2, 1982. a, b, c
Boers, R. and Mitchell, R. M.: Absorption feedback in stratocumulus clouds influence on cloud top albedo, Tellus A, 46, 229–241, 1994. a, b, c, d
Short summary
The article presents a new conceptual model to describe the temporal evolution of continental fog layers, developed based on 7 years of fog measurements performed at the SIRTA observatory, France. This new paradigm relates the visibility reduction caused by fog to its vertical thickness and liquid water path and provides diagnostic variables that could substantially improve the reliability of fog dissipation nowcasting at a local scale, based on real-time profiling observation.
Final-revised paper