TY - JOUR
T1 - A Numerical Study of Turbulence Statistics and the Structure of a Spatially-Developing Boundary Layer Over a Realistic Urban Geometry
AU - Inagaki, Atsushi
AU - Kanda, Manabu
AU - Ahmad, Nurul Huda
AU - Yagi, Ayako
AU - Onodera, Naoyuki
AU - Aoki, Takayuki
N1 - Publisher Copyright:
© 2017, Springer Science+Business Media Dordrecht.
PY - 2017/8/1
Y1 - 2017/8/1
N2 - The applicability of outer-layer scaling is examined by numerical simulation of a developing neutral boundary layer over a realistic building geometry of Tokyo. Large-eddy simulations are carried out over a large computational domain (19.2km×4.8km×1km in the streamwise, spanwise, and vertical directions, respectively), with a fine grid spacing (2 m) using the lattice-Boltzmann method with massively parallel graphics processing units. The simulation produces a ratio of the boundary-layer height to the average building height of more than 50. Results from simulations show that outer-layer features are maintained for turbulence statistics in the upper part of the boundary layer, as well as the width of predominant streaky structures throughout the entire boundary layer, despite the very large roughness. This is caused by the existence of very large streaky structures extending throughout the entire boundary layer, which follow outer-layer scaling with a self-preserving development. We assume the top-down mechanism in the physical interpretation of results.
AB - The applicability of outer-layer scaling is examined by numerical simulation of a developing neutral boundary layer over a realistic building geometry of Tokyo. Large-eddy simulations are carried out over a large computational domain (19.2km×4.8km×1km in the streamwise, spanwise, and vertical directions, respectively), with a fine grid spacing (2 m) using the lattice-Boltzmann method with massively parallel graphics processing units. The simulation produces a ratio of the boundary-layer height to the average building height of more than 50. Results from simulations show that outer-layer features are maintained for turbulence statistics in the upper part of the boundary layer, as well as the width of predominant streaky structures throughout the entire boundary layer, despite the very large roughness. This is caused by the existence of very large streaky structures extending throughout the entire boundary layer, which follow outer-layer scaling with a self-preserving development. We assume the top-down mechanism in the physical interpretation of results.
KW - Lattice-Boltzmann method
KW - Outer-layer scaling
KW - Top-down mechanism
KW - Urban boundary layer
KW - Very large streaky structures
UR - http://www.scopus.com/inward/record.url?scp=85018313804&partnerID=8YFLogxK
U2 - 10.1007/s10546-017-0249-y
DO - 10.1007/s10546-017-0249-y
M3 - Article
AN - SCOPUS:85018313804
SN - 0006-8314
VL - 164
SP - 161
EP - 181
JO - Boundary-Layer Meteorology
JF - Boundary-Layer Meteorology
IS - 2
ER -