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. 2017 Jun 8;164(3):337–351. doi: 10.1007/s10546-017-0258-x

Table 1.

Details of the various datasets used

Case Method Acronym: Authors H / h Δ/h
Staggered cubes DNS LC: Leonardi and Castro (2010) 8.0 1/100
Staggered and aligned cubes DNS CTCB: Coceal et al. (2006) 8.0 1/32
Staggered and aligned cubes DNS BCTB: Branford et al. (2011) 8.0 1/32
Staggered cubes, various angles LES CCTBBC: Claus et al. (2012) 4.0 1/25
Staggered, random height LES XCC: Xie et al. (2008) 10.0 1/16
Aligned cubes (b.layer) LES CP-A: Cheng and Porte-Agel (2015)  12 1/16
Staggered and aligned cubes (b.layer) LES YSMM: Yang et al. (2016) 24 1/8
Aligned h×2h×h blocks DNS, LES CXFRCHHC: Castro et al. (2016) 12 1/12

Except for CP-A’s and YSMM’s LES, where H refers to the approximate boundary-layer depth, all cases were channel-flow computations, with H the channel half-height. All cases except CCTBBC and CXFRCHHC considered only arrays that were flow-aligned—i.e. wind direction normal to the faces of the obstacles. For the LES cases, the subgrid models used were either the standard Smagorinsky model (CCTBBC, XCC, CXFRCHHC), the modulated gradient model of Lu and Porte-Agel (2010) (CP-A), or the Vreman (2010) model (YSSM)