Ground-Based Observations and Modeling of the Visibility and Radar Reflectivity in a Radiation Fog Layer

• Published in: Journal of atmospheric and oceanic technology Vol. 30; no. 2; pp. 288 - 300
• Main Authors: Boers, R, Baltink, HKlein, Hemink, HJ, Bosveld, F C, Moerman, M
• Format: Journal Article
• Language: English
• Published: Boston American Meteorological Society 01.02.2013
• Subjects: Aerosols; Air traffic control; Atmospheric research; Atmospheric sciences; Clouds; Droplets; Evaporation; Fog; Marine; Meteorology; Radar; Radar systems; Reflectivity; Remote sensing; Supersaturation; Traffic accidents & safety; Visibility; Water vapor; Netherlands, Utrecht, Cabauw
• ISSN: 0739-0572; 1520-0426
• DOI: 10.1175/JTECH-D-12-00081.1

The development of a radiation fog layer at the Cabauw Experimental Site for Atmospheric Research (51.97 degree N, 4.93 degree E) on 23 March 2011 was observed with ground-based in situ and remote sensing observations to investigate the relationship between visibility and radar reflectivity. The fog layer thickness was less than 200 m. Radar reflectivity values did not exceed -25 dBZ even with visibilities less than 100 m. The onset and evaporation of fog produce different radar reflectivity-visibility relationships. The evolution of the fog layer was modeled with a droplet activation model that used the aerosol size distribution observed at the 60-m altitude tower level as input. Radar reflectivity and visibility were calculated from model drop size spectra using Mie scattering theory. Since radiative cooling rates are small in comparison with cooling rates due to adiabatic lift of aerosol-laden air, the modeled supersaturation remains low so that few aerosol particles are activated to cloud droplets. The modeling results suggest that the different radar reflectivity-visibility relationships are the result of differences in the interplay between water vapor and cloud droplets during formation and evaporation of the fog. During droplet activation, only a few large cloud droplets remain after successfully competing for water vapor with the smaller activated droplets. These small droplets eventually evaporate (deactivate) again. In the fog dissolution/evaporation stage, only these large droplet need to be evaporated. Therefore, to convert radar reflectivity to visibility for traffic safety products, knowledge of the state of local fog evolution is necessary.