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- W2584623035 abstract "Selected modeling and observational studies on the role of turbulence on marine fog formation are introduced. There can be basically three types of marine fog. Advection fog forms usually when turbulence generated by wind shear or longwave radiative cooling plays a crucial role in cooling and moistening the air above a cold sea surface after the advection of warm and moist air. In contrast, steam fog would be generated by the turbulence which plays an important role in transporting moisture from a relatively warm sea surface. The transition of stratus cloud into marine fog is another formation mechanism. The bottom of marine stratus clouds can be lowered to form marine fog by the cooling of the air just below the cloud base caused by turbulent heat loss and droplet evaporation, which can also supply moisture. Moreover, stratus cloud top can descend owing to the evaporation of cloud droplets in this region by entrainment of warm and dry air from above the cloud top under strong subsidence." @default.
- W2584623035 created "2017-02-10" @default.
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- W2584623035 date "2017-01-01" @default.
- W2584623035 modified "2023-09-27" @default.
- W2584623035 title "Turbulence in Marine Fog" @default.
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- W2584623035 doi "https://doi.org/10.1007/978-3-319-45229-6_4" @default.
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