Abstract
The utilization of windbreaks is a globally prevailing management practice for agricultural production and restoration of degraded ecosystems by reducing wind-induced destruction. Examining how windbreaks affect leeward surface wind speed is critically important to quantify the efficiency of windbreaks. A semiempirical model for simulating horizontal distribution of wind speed leeward windbreaks was developed, combining wind tunnel experiments with prevailing literature. The model simulated the horizontal leeward wind speed distribution windbreaks with acceleration and deceleration terms; simultaneously considering four key impact factors (windbreak aerodynamic porosity, surface roughness, Richardson number and wind incident angle). It also comprises of a simple quantitative method for determining windbreak aerodynamic porosity from optical porosity. Model results compared with published data illustrate that the model is robust in various wind speed distributions under different windbreak structures and turbulence conditions. The simulation results indicate horizontal wind speed distribution is definitely dependent upon windbreak porosity. Wind speeds decline with increasing wind incident angle. Wind speeds decrease obviously with increasing Richardson number while decrease slightly with decreasing surface roughness, when the horizontal distance is between two and twenty times the windbreak height. Moreover, the escalating wind incident angle strengthens the weakening effects of windbreak porosity on wind speed, while reducing Richardson numbers expand the decreasing intervals of relative wind speed with increasing surface roughness. The model provides a simple and practical method to better assess the impacts of windbreaks, which can be incorporated in agricultural policy-making decisions to reduce the detrimental impacts of wind.
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Abbreviations
- α :
-
Aerodynamic porosity (0-1)
- β :
-
Optical porosity (0-1)
- μ 0 :
-
The mean horizontal wind speed in the open (m/s)
- μ x :
-
The mean horizontal wind speed at the horizontal distance of x (m/s)
- μx/μ0 :
-
Wind speed relative to open (0-1)
- z 0 :
-
Surface roughness length
- z0/H :
-
Surface roughness
- H :
-
Windbreak height (m)
- L :
-
Obukhov length
- R h :
-
Richardson number
- θ :
-
Incident angle of the wind (°)
- b1, b2 :
-
Model parameters
- k1, k2 :
-
Model parameters
- f 1 :
-
The acceleration-term function indicated the convergence of the falling air to the surface airflow
- f 2 :
-
The deceleration-term function indicated the diffusion of airflow after progressing through the windbreak
- x :
-
The horizontal distance along the normal to the windbreak and expressed in terms of windbreak height (H)
- ξ :
-
Influential factors represented α, Rh and z0/H
- ϕi(α):
-
Aerodynamic porosity influential function for parameter b
- Φi(α):
-
Aerodynamic porosity influential function for parameter k
- λi(Rh):
-
Atmospheric stability influential function for parameter b
- Λi(Rh):
-
Atmospheric stability influential function for parameter k
- ηi(z0):
-
Surface roughness influential function for parameter b
- χi(z0):
-
Surface roughness influential function for parameter k
- R a :
-
Results of model responses for altered variables
- R n :
-
Results of model responses for nominal variables
- V a :
-
The altered variables
- V n :
-
The nominal variables
- S :
-
The sensitivity index
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Acknowledgements
We are grateful for the constructive comments from two anonymous reviewers. Dr. Changjie Jin made valuable comments in early version of this manuscript. XX is grateful for the financial and facility support from the San Diego State University.
Funding
This work was supported by Forestry Ecological Science and Technology Project of China (Grant No.: 2015BAD07B0505) and National Natural Science Foundation of China (31400541).
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Yuan, F., Wu, J., Wang, A. et al. A semiempirical model for horizontal distribution of surface wind speed leeward windbreaks. Agroforest Syst 94, 499–516 (2020). https://doi.org/10.1007/s10457-019-00417-0
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DOI: https://doi.org/10.1007/s10457-019-00417-0