Large-Eddy Simulations on the Effects of Surface Geometry of Building Arrays on Turbulent Organized Structures

By M. Kanda. 2004

209 citations recorded by the source corpus.

Subfields: Computational Mechanics, Environmental Engineering, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/0f4a5c63bb5d97617e318fbdd4a8960b789b1e5f

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 Environmental Engineering

In Global and Planetary Change

Citations in the corpus

Channel flow over large cube roughness: a direct numerical simulation study (2010, result): “Note that these results are consistent with the finding that for arrays of random (or at least multiple) height obstacles, the surface stress is dominated by the form drag of the tallest obstacles (see Kanda 2006; Xie et al. 2008).”
Coherent Structures and the Dissimilarity of Turbulent Transport of Momentum and Scalars in the Unstable Atmospheric Surface Layer (2011, background): “Hommema and Adrian 2003; Carper and Porte-Agel 2004; Kanda 2006; Huang et al. 2009; Inagaki and Kanda 2010; Horiguchi et al. 2010).”
Large-Eddy Simulation of Flows over Random Urban-like Obstacles (2008, unknown): “In eld studies (see Kastner-Kline & Rotach, 2004, for an example) such randomness is of course virtually guaranteed but its eects on the nature of the ow, as compared with ows over uniform, regular obstacle arrays, have seem not to have been explicitly investigated, apart from the recent study by K”
Aerodynamic Parameters of Regular Arrays of Rectangular Blocks with Various Geometries (2009, background): “Such a clear peak of Cd for cubical staggered arrays is consistent with both the results from LES by Kanda (2006) and results from the k–e model used by Santiago et al. (2008) despite their drag coefficients being defined using the wind within the urban canopy layer.”
Large-Eddy Simulation of the Atmospheric Boundary Layer (2020, methodology): “In physical LES, the large scales of the flow (i.e., large eddies) are computed explicitly on the numerical mesh, while the effects of the small scales are modelled (Pope 2004).”
Roughness Lengths for Momentum and Heat Derived from Outdoor Urban Scale Models (2007, methodology): “6. c. Seasonal and diurnal variations of lnzh Large diurnal variations of lnzh (or B 1) have been observed in the past for sparse vegetation (e.g., see review by Verhoef et al. 1997) and urban areas (Voogt and Grimmond 2000; Moriwaki and Kanda 2006).”