Boundary layer turbulence refers to the chaotic, swirling motions that occur within the lowest part of the atmosphere, known as the boundary layer, due to surface heating, wind shear, and surface roughness. These turbulent motions play a crucial role in mixing air, heat, moisture, and momentum between the Earth's surface and the atmosphere. Fluxes describe the transfer rates of these properties, driven by turbulence, which significantly influence weather, climate, and air quality.
Boundary layer turbulence refers to the chaotic, swirling motions that occur within the lowest part of the atmosphere, known as the boundary layer, due to surface heating, wind shear, and surface roughness. These turbulent motions play a crucial role in mixing air, heat, moisture, and momentum between the Earth's surface and the atmosphere. Fluxes describe the transfer rates of these properties, driven by turbulence, which significantly influence weather, climate, and air quality.
What is boundary layer turbulence?
Turbulent, chaotic air motions in the lowest part of the atmosphere (the atmospheric boundary layer) driven by surface heating, wind shear, and surface roughness, which mix air vertically.
What causes boundary layer turbulence?
Surface heating that promotes rising air, wind shear (variation of wind with height), and rough surfaces (terrain, vegetation, buildings) that roughen the flow and generate eddies.
What are the main fluxes in the boundary layer?
Momentum, sensible heat, and latent heat fluxes, transported by turbulent eddies between the surface and the air.
Why does boundary layer turbulence matter for weather and climate?
It controls how heat, moisture, and momentum mix near the surface, affecting temperatures, humidity, cloud formation, pollutant dispersion, and the overall energy and moisture budgets that drive weather and climate.