Double-averaging methodology and its application to turbulent flow in and above vegetation canopies
By J. Finnigan, R. Shaw. 2008
51 citations recorded by the source corpus.
Subfields: Computational Mechanics, Environmental Engineering, Global and Planetary Change
View Paper: https://www.semanticscholar.org/paper/63eaedd0e06bb68f54fa104f36893c4eaed76fd0
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In Computational Mechanics
In Environmental Engineering
In Global and Planetary Change
Citations in the corpus
- Review of wave‐turbulence interactions in the stable atmospheric boundary layer (2015, background): “…between waves and turbulence can be investigated through decomposing atmospheric variables into a time-averaged mean flow and wavelike and turbulent components [Fua et al., 1982; Einaudi et al., 1984; Finnigan et al., 1984; Finnigan, 1988; Einaudi and Finnigan, 1993; Finnigan and Shaw, 2008].”
- Turbulence structure above a vegetation canopy (2009, background): “Flow statistics are formed by averaging first in time and then spatially over the volume V (Raupach & Shaw 1982; Finnigan 1985; Raupach, Coppin & Legg 1986; Brunet, Finnigan & Raupach 1994; Finnigan & Shaw 2008).”
- A Note on Two-Equation Closure Modelling of Canopy Flow (2009, background): “Raupach and Shaw 1982; Finnigan 2000; Finnigan and Shaw 2008 ).”
- The Explicit Wake Parametrisation V1.0: a wind farm parametrisation in the mesoscale model WRF (2015, methodology): “Approach 1 follows Raupach and Shaw (1982) and Finni- gan and Shaw (2008) and defines MKE = 1 2 〈u2i 〉 = 1 2 〈ui 〉 2 + 1 2 〈u′′i 2 〉 and TKE = 1 2 〈u′i 2 〉.”