Coastal-fog microphysics using in-situ observations and GOES-R retrievals

• Published in: Boundary-Layer Meteorology
• Other Authors: Gultepe, I. (author), Pardyjak, E. (author), Hoch, S. W. (author), Fernando, H. J. S. (author), Dorman, C. (author), Flagg, D. D. (author), Krishnamurthy, R. (author), Wang, Q. (author), GaberÅ¡ek, S. (author), Creegan, E. (author), Scantland, N. (author), Desjardins, S. (author), Heidinger, A. (author), Pavolonis, M. (author), Heymsfield, Andrew J. (author)
• Format: Article in Journal/Newspaper
• Language: English
• Published: 2021
• Subjects: Newfoundland
• Online Access: https://doi.org/10.1007/s10546-021-00622-4

The objective of this work is to evaluate GOES-R (Geostationary Operational Environmental Satellites-R series) data-based fog conditions which occurred during the C-FOG (Toward Improving Coastal Fog Prediction) field campaign. The C-FOG campaign was designed to advance understanding of fog formation, development, and dissipation over coastal environments to improve predictability. The project took place along coastlines and open water environments of eastern Canada (Nova Scotia, and the Island of Newfoundland) during August-October of 2018 where environmental conditions play an important role for late season fog formation. During the C-FOG field campaign, coastal instruments were mainly located at the Ferryland supersite, Newfoundland, with two main sites, and five satellite sites, as well as on the Research Vessel Hugh R. Sharp. Key in-situ measurement instruments included microphysical, meteorological, radiation, and aerosol sensors. A fog spectral probe was used for measuring droplet spectra from 1-50 mu m at the Ferryland supersite. A laser precipitation monitor with 100 mu m to 10 mm size range and an optical particle counter with 0.3-17 mu m at 16 spectral channels provided information for fog and drizzle discrimination. Remote sensing platforms, e.g. profiling microwave radiometer, ceilometer, microwave rain radar, lidar, meteorological towers, tethered balloons, and GOES-R products for fog coverage, and droplet size and liquid water path) were used to evaluate fog over horizontal and vertical dimensions. Results suggest that effective radius, phase, liquid water path, and liquid water content values obtained from GOES-R and the profiling microwave radiometer are comparable to ground-based in-situ observations. It is concluded that integration of observations and nowcasting products may help improve short-term local fog predictions.