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Fog Formation Related to Gravity Currents Interacting with Coastal Topography



Details

  • Journal Title:
    Boundary-Layer Meteorolgy
  • Personal Author:
  • NOAA Program & Office:
  • Description:
    An interesting mixing-fog event was identified during the C-FOG field campaign, where a cold-frontal airmass arriving from the north-east collided with The Downs peninsula in Ferryland, Newfoundland, Canada, to produce misty/foggy conditions. A comprehensive set of field observations suggests that this collision caused turbulent mixing of nearly saturated ambient air with an almost saturated cold-frontal airmass, creating conditions for mixing fog. To delve into the physical processes underlying this phenomenon, laboratory experiments were performed on the interaction of lock-exchange-induced gravity currents with a rectangular obstacle. Instantaneous velocity and density fields were obtained using particle image velocimetry and planar laser-induced fluorescence. The observations suggest that the obstacle starts affecting the approaching gravity-current propagation at an upstream distance of 2H and, upon collision, the mixing occurs over a length of 0.83H, where H is the depth of the ambient fluid layer. The time for larger-scale turbulent stirring to permeate to the smallest scales of turbulence and activate the condensation nuclei is estimated as 3t∗, where t∗=H/g′−−−−√ is the intrinsic time scale of the gravity current, and g′ is the reduced gravity. Extrapolation of laboratory results to field conditions shows a good agreement with observations.
  • Keywords:
  • Source:
    Boundary-Layer Meteorol 181, 499-521
  • DOI:
  • Document Type:
  • Rights Information:
    Accepted Manuscript
  • Compliance:
    Submitted
  • Main Document Checksum:
    urn:sha256:f06e9af3634a97dcab4b9e85d26c727ebde2dcf7a2134940d52771b68b7b52d4
  • Download URL:
  • File Type:
    Filetype[PDF - 1.83 MB ]
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