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Bioclimatic schemes 02

1:100 Scale dwg file (meters)
Conversion from meters to feet: a fast and fairly accurate system consists in scaling the drawing by multiplying the value of the unit of measurement in meters by 3.281
 

Scheme on the interactions between soil and atmosphere
The diagram shows the diurnal evolution of the structure of the atmospheric boundary layer (Stull 1988)
      – Scrambled 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, close to the surface. The turbulence is homogeneous, different from the rest of           the planetary limit state.

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