GetWind: Get the average wind speed at center of canopy layer

Description Usage Arguments Details Value References Examples

View source: R/0-Functions.R

Description

Calculate the wind speed decrease in two steps:

  1. Decrease the measured wind speed from measurement height until top of the canopy using the formulation of Van de Griend and Van Boxel (1989)

  2. Decrease wind speed further with increasing canopy depth using an exponential extinction coefficient and a cumulated LAI above the target point.

Usage

 1
 2
 3
 4
 5
 6
 7
 8
 9
10
11
12
13
GetWind(
  Wind,
  LAI_lay,
  LAI_abv,
  extwind = 0,
  Z_top,
  ZHT,
  Z0 = Z_top * 0.1,
  ZPD = Z_top * 0.75,
  alpha = 1.5,
  ZW = ZPD + alpha * (Z_top - ZPD),
  vonkarman = Constants()$vonkarman
)

Arguments

Wind

Above canopy wind speed (m s-1)

LAI_lay

Leaf area index of the layer (m2 leaves m-2 soil)

LAI_abv

Cumulated leaf area index above the layer (m2 leaves m-2 soil)

extwind

Extinction coefficient. Default: 0, no extinction.

Z_top

Average canopy height of the taller crop (m)

ZHT

Wind measurement height (m)

Z0

Roughness length (m). Default: 0.1*Z_top

ZPD

Zero-plane displacement (m), Default: 0.75*Z_top

alpha

Constant for diffusivity at top canopy. Default: 1.5 following Van de Griend et al (1989).

ZW

Top height of the roughness sublayer (m). Default: ZPD+alpha*(Z2-ZPD)

vonkarman

Von Karman constant, default to Constants()$vonkarman, 0.41.

Details

The function computes the average wind speed at the center of the canopy layer. It is considered that the leaf distibution is homogeneous in the layer, so the LAI_lay parameter is used to add half of the target layer to the cumulated LAI above:

WindLay= Wh*e(-extwind*(LAI_abv+LAI_lay/2)

with Wh the wind speed at top of the canopy. Note: the alpha parameter can also be computed as:

alpha= (zw-d)/(Z2-d)

Value

WindLay

The winspeed at the center of the layer (m s-1)

References

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. Part of the code is taken from the MAESPA model.

Examples

1
2
# Windspeed in a coffee layer managed in agroforestry system
GetWind(Wind=3,LAI_lay=4,LAI_abv=0.3,extwind= 0.58,Z_top = 24,ZHT = 25)

VEZY/DynACof documentation built on Feb. 3, 2021, 8:52 p.m.