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Bioclimatic Schemes 02
Dwg file at 1:100 scale (meters)
Diagram of soil-atmosphere interactions
The diagram shows the diurnal evolution of the structure of the atmospheric boundary layer (Stull 1988)
- Mixed layer: heated from below, thermal and mechanical turbulence.
- Stable layer: the temperature increases with altitude, so it is very stable (little mixed).
- Residual layer: neutral stratification; can trap pollutants until the next day
- Surface layer: 10% of the planetary boundary layer, near the surface. The turbulence is homogeneous, different from the rest of the planetary boundary state.
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