under which condition does advection fog usually form

In addition, it was confirmed that the difference in SST resolution led to varying sizes and strengths of the warm pools that provided water vapor from the open sea area to the atmosphere. RTG-SST was successful at identifying fog presence and maintained the most extensive horizontal distribution of cold water masses. While conventional analyses have used initial SST distributions throughout the entire simulation period, small-scale, rapidly developing oceanic phenomena (e.g., cold water masses) lasting for several days act as an important mediating factor between the lower atmosphere and sea. Data from the Final Operational Model Global Tropospheric Analyses were provided at 1° and 0.25° resolutions and NOAA real-time global SST (RTG-SST) data were provided at 0.083°. The present study aimed to analyze the differences in cold water mass formation according to sea surface temperature (SST) resolution and its effects on the occurrence and distribution of sea fog over the Korean Peninsula from June 23–July 1, 2016, according to the Weather Research and Forecasting model. In particular, marine fog driven by summer cold water masses can inhibit transport and aviation yet a lack of observational data hinders our understanding of this phenomena. Recent rapid industrial development in the Korean Peninsula has increased the impacts of meteorological disasters on marine and coastal environments.

Under which condition does advection fog usually form