WIND DIRECTION PROFILES IN INTERFACE
For both the CBL & SBL wind direction is assumed to be constant with height both above the highest and below the lowest measurements. For intermediate heights, AERMOD linearly interpolate between measurements.
4 AERMOD’s Meteorological Interface
4.1
General Profiling Equations
4.1.1
WIND SPEED PROFILING IN THE INTERFACE
4.1.2
WIND DIRECTION PROFILES IN INTERFACE
4.1.3
PROFILES OF THE POTENTIAL TEMPERATURE GRADIENT IN THE
INTERFACE
4.1.4
POTENTIAL TEMPERATURE PROFILING IN THE INTERFACE
4.1.5
VERTICAL TURBULENCE CALCULATED BY THE INTERFACE
4.1.6
LATERAL TURBULENCE CALCULATED BY THE INTERFACE
4.2
Vertical Inhomogeneity in the Boundary Layer as Treated by the INTERFACE
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