Two years subsequent to the field campaign, significant advancements have been made across multiple research fronts, and they are: 1) Analysis of high-resolution field observations during Intensive Observation Periods (IOPs) have enabled the identification of near-surface and boundary layer conditions conducive to cold fog formation. Notably, atmospheric turbulence conditions near the surface were characterized for the first time in the context of mountainous cold fog. Additionally, the thermodynamic circulation governing moisture transfer and fog formation was investigated. 2) Utilizing a diverse array of instruments, the microphysical evolution of cold fog, particularly ice fog, was comprehensively characterized. This included studying the relationship between heat and moisture budgets during fog events observed, with a focus on particle (including droplets) spectra. 3) Air chemistry and aerosol measurements were employed to investigate "new particle formation" processes occurring within the fog environment. 4) Applying the rich field data facilitated unprecedented opportunities to validate high-resolution numerical weather prediction models. In this respect, large-eddy simulations of fog events and the sub-km scale prediction were conducted, highlighting the necessity of accurately predicting local ephemeral fog events using very high resolution simulations. 5) Identifying strategies for assimilating high-resolution field campaign data using advanced data assimilation methods.
This presentation will highlight the progress made in the mentioned research areas, presenting new findings, and sample results obtained through the analysis of CFACT project data.
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