Turbulence in plant canopies

By J. Finnigan. 2000

1,690 citations recorded by the source corpus.

Subfields: Computational Mechanics, Earth-Surface Processes, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/5f7cb077b00b70114cd83c2968d7ae1a5cd2ac6d

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Computational Mechanics

In Earth-Surface Processes

In Global and Planetary Change

Citations in the corpus

Drag force parameters of rigid and flexible vegetal elements (2015, background): “…to characterize the drag of vegetation [Nepf, 1999; Poggi et al., 2004; Nezu and Sanjou, 2008; Aberle and J€arvel€a, 2013] in liquid and air [Finnigan, 2000; de Langre, 2008], and comparisons between obstructions with different flexibilities have been studied [Ghisalberti and Nepf, 2006;…”
Structure of turbulent flow over regular arrays of cubical roughness (2007, methodology): “Over very rough walls, the viscous sublayer is effectively replaced by the roughness sublayer (Raupach, Antonia & Rajagopalan 1991); it is the roughness itself, rather than any viscous layers attached to it, that provides the dominant mechanism for generating near-wall turbulence.”
Mechanisms of long-distance dispersal of seeds by wind (2002, methodology): “Closure models, and the mixing layer analogy that describes key length and timescales of organized eddy motion for canopy flows, have been reviewed by Finniga”
A Re-Evaluation of Long-Term Flux Measurement Techniques Part I: Averaging and Coordinate Rotation (2003, background): “The reason for this change in scaling behaviour is the different mechanism of turbulence generation that obtains in the roughness sublayer compared to the surface layer (Raupach et al., 1996; Finnigan, 2000).”
Modeling Turbulent Flows in Porous Media (2020, methodology): “Because of phase boundaries, the operations of spatial differentiation and spatial averaging do not, in general, commute; these are handled by application of the spatial averaging theorem (Whitaker 1999, Finnigan 2000), 〈∇ ⊗ u〉|(x,t ) =∇ ⊗ 〈u〉 + ∫ r∈Aγ κ G(r − x)nγ κ (r) ⊗ u(r, t ), dA(r), 8.”
ONE- and TWO-Equation Models for Canopy Turbulence (2004, background): “Given that lm reflects known bulk characteristics of canopy eddies (Raupach et al., 1996; Katul et al., 1998; Finnigan, 2000), and noting the large uncertainty in the e models, mt 1⁄4 m t appears to be rational.”
Stably Stratified Atmospheric Boundary Layers (2014, background): “Short-circuiting of canopy turbulence is discussed in Finnigan (2000).”
Review of wave‐turbulence interactions in the stable atmospheric boundary layer (2015, background): “Vorticity waves associated with inflection points in the wind profile are routinely observed near velocity jets and canopy tops [e.g., Raupach et al., 1996; Lee, 1997; Lee et al., 1997; Lee and Barr, 1998; Finnigan, 2000; Finnigan et al., 2009].”
Modeling the interaction between flow and highly flexible aquatic vegetation (2010, methodology): “Where many models for flow through vegetation have used principles derived from studies on atmospheric boundary layer flow [Finnigan, 2000; Poggi et al., 2004], our model also uses principles of flow through porous media [cf.”
A Note on Two-Equation Closure Modelling of Canopy Flow (2009, background): “The foliage-related terms are inherently different and can be derived systematically from the momentum equations, with proper attention to the necessity for spatial averaging over the multiply-connected canopy airspace (e.g. Raupach and Shaw 1982; Finnigan 2000; Finnigan and Shaw 2008).”
A Note On The Contribution Of Dispersive Fluxes To Momentum Transfer Within Canopies (2004, methodology): “The most poorly understood terms in the time and horizontally averaged momentum equation are the dispersive fluxes (Raupach, 1994; Finnigan, 2000); these terms are the subject of the present investigation.”
Shear instability and coherent structures in shallow flow adjacent to a porous layer (2007, positive): “However, there is a significant body of literature on turbulence above terrestrial forest and aquatic seagrass canopies (Raupach, Finnigan & Brunet 1996; Finnigan 2000; Nepf & Vivoni 2000).”
Effects of Wind on Plants (2008, background): “Previous surveys in this series (Raupach & Thom 1981, Finnigan 2000) focused on the effect of vegetation on wind, in particular on its turbulent features, rather than on the reverse.”