Wind-Tunnel Study Of Atmospheric Stable Boundary Layers Over A Rough Surface

By Y. Ohya. 2001

159 citations recorded by the source corpus.

Subfields: Atmospheric Science, Computational Mechanics, Environmental Engineering

View Paper: https://www.semanticscholar.org/paper/3f9dd38c243e3bc4f17ea9ce7171a04a90828b5b

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Citations in the corpus

Turbulence energetics in stably stratified geophysical flows: Strong and weak mixing regimes (2008, methodology): “1 < Ri < 100); green – laboratory sheared flow (Ohya, 2001);”
A Wind-Tunnel Investigation of Wind-Turbine Wakes: Boundary-Layer Turbulence Effects (2009, methodology): “A similar roughness configuration was recently used by Ohya (2001) to study stable boundary layers over rough surfaces.”
Energy- and flux-budget (EFB) turbulence closure model for stably stratified flows. Part I: steady-state, homogeneous regimes (2006, background): “Fig. 2 Same as in Fig. 1 but for the squared dimensionless turbulent fluxes of (a) momentum, ˆ τ 2 = (τ/E K )2 ,a nd (b) potential temperature, ˆ F 2 z = F 2 z /(E K Eθ ), based on laboratory experiments: diamonds ( Ohya 2001 ) and LES: triangles (new data provided by Igor Esau); and meteorological ”
A Hierarchy of Energy- and Flux-Budget (EFB) Turbulence Closure Models for Stably-Stratified Geophysical Flows (2011, background): “1997); laboratory experiments: slanting crosses (Rehmann and Koseff 2004), diamonds (Ohya 2001), black circles (Strang and Fernando 2001); DNS: five-pointed stars (Stretch et al.”
Wind-Turbine Wakes in a Convective Boundary Layer: A Wind-Tunnel Study (2013, unknown): “Specifically, physical simulations of thermally stratified boundary layers have been carried out by e.g., Meroney and Melbourne (1992), Fedorovich et al. (1996), Ohya (2001), Ohya and Uchida (2004), Chamorro and Porté-Agel (2010), and Hancock and Pascheke (2010).”
Stable-boundary-layer regimes from the perspective of the low-level jet (2008, background): “This dependence of profile shape on stability has also been noted in wind-tunnel studies of the stably stratified BL (Ohya et al. 1997, Ohya 2001).”
Turbulent Velocity-Variance Profiles in the Stable Boundary Layer Generated by a Nocturnal Low-Level Jet (2006, background): “(1993) and in the wind tunnel (Ohya et al. 1997; Ohya 2001) show diminished but distinctly nonzero values of turbulence at the SBL top.”