Turbulence structure above a vegetation canopy

By J. Finnigan, R. Shaw, E. Patton. Journal of Fluid Mechanics, 2009

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The Parallelized Large-Eddy Simulation Model (PALM) version 4.0 for atmospheric and oceanic flows: model formulation, recent developments, and future perspectives (2015, methodology): “…applied by various authors to study turbulent ﬂows inside and above homogeneous as well as heterogeneous canopies such as forest edges (Cassiani et al., 2008; Finnigan et al., 2009; Dupont and Brunet, 2009, among others In case of incoming solar radiation the plant canopy acts as a source of heat .”
Review of wave‐turbulence interactions in the stable atmospheric boundary layer (2015, background): “D beyond its original definition to include cases with N ≠ 0, e.g., for flow over canopy top [e.g., Hu et al., 2002; Finnigan et al., 2009; Belcher et al., 2012].”
Large-Eddy Simulation of the Atmospheric Boundary Layer (2020, methodology): “In a follow up, Bailey and Stoll (2016) used a similar simulation configuration to Finnigan et al. (2009) but with structure identification from the full velocity gradient tensor (e.g., λ2 following Jeong and Hussain 1995).”