Description Usage Arguments Details Value References See Also Examples
Compute the aerodynamic conductance for sensible and latent heat between the center of the lowest canopy layer and the soil surface following Van de Griend and Van Boxel (1989).
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Wind |
Average daily wind speed above canopy (m s-1) |
ZHT |
Wind measurement height (m) |
Z_top |
Average canopy height of the taller crop (m) |
Z0 |
Roughness length (m). Default: |
ZPD |
Zero-plane displacement (m), Default: |
alpha |
Constant for diffusivity at top canopy. Default: |
ZW |
Top height of the roughness sublayer (m). Default: |
LAI |
Total leaf area index above the soil (m2 leaf m-2 soil). |
extwind |
Extinction coefficient. Default: |
vonkarman |
Von Karman constant, default to |
alpha
can also be computed as:
alpha= (zw-d)/(Z_top-d)
The aerodynamic conductance between the lowest canopy layer and the soil is computed as:
g_a0= 1/((Uh/Kh)*log(U_mid/U_0))
where U_mid is the wind speed at median cumulated LAI between the top and the soil, and U_0 the wind speed at soil surface.
g_a0 |
The aerodynamic conductance of the air between the lowest canopy layer and the soil surface (m s-1) |
Van de Griend, A.A. and J.H. Van Boxel, Water and surface energy balance model with a multilayer canopy representation for remote sensing purposes. Water Resources Research, 1989. 25(5): p. 949-971.
G_bulk()
and GetWind()
, which is used internaly.
1 2 | # G_a0 for a coffee plantation managed in agroforestry system:
G_soilcan(Wind= 1, ZHT= 25, Z_top= 24,LAI= 4.5, extwind= 0.58)
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