On the effect that the direction of geostrophic wind has on turbulence and quasiordered large-scale structures in the atmospheric boundary layer

Author:

Glazunov A. V.

Publisher

Pleiades Publishing Ltd

Subject

Atmospheric Science,Oceanography

Reference36 articles.

1. S. Hoyas and J. Jimenez, “Scaling of the Velocity Fluctuations in Turbulent Channels up to Reτ = 2003,” Center for Turbulence Research Annual Research Briefs, 351–356 (2005).

2. A. V. Glazunov, “Large-Eddy Simulation of Turbulence with the Use of a Mixed Dynamic Localized Closure: Part 1. Formulation of the Problem, Model Description, and Diagnostic Numerical Tests,” Izv. Akad. Nauk, Fiz. Atmos. Okeana 45(1), 7–28 (2009) [Izv., Atmos. Ocean. Phys. 45 (1), 5–24 (2009)].

3. A. V. Glazunov, “Large-Eddy Simulation of Turbulence with the Use of a Mixed Dynamic Localized Closure: Part 2. Numerical Experiments: Simulating Turbulence in a Channel with Rough Boundaries,” Izv. Akad. Nauk, Fiz. Atmos. Okeana 45(1), 29–42 (2009) Izv. Akad. Nauk, Fiz. Atmos. Okeana 45 (1), 25–36 (2009)].

4. B. J. Balakumar and R. J. Adrian, “Largeand Very Large-Scale Motions in Channel and Boundary-Layer Flows,” Philos. Trans. R. Soc. London Ser. A 365 665–681 (2007).

5. I. Esau, “The Coriolis Effect on Coherent Structures in Planetary Boundary Layers,” J. Turbulence 4(1), 17 (2003).

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