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Implementation of a synthetic inflow turbulence generator in idealised WRF v3.6.1 large eddy simulations under neutral atmospheric conditions

Implementation of a synthetic inflow turbulence generator in idealised WRF v3.6.1 large eddy simulations under neutral atmospheric conditions
Implementation of a synthetic inflow turbulence generator in idealised WRF v3.6.1 large eddy simulations under neutral atmospheric conditions
A synthetic inflow turbulence generator was implemented in the idealised Weather Research and Forecasting large eddy simulation (WRF-LES v3.6.1) model under neutral atmospheric conditions. This method is based on an exponential correlation function, and generates a series of two-dimensional slices of data which are correlated both in space and in time. These data satisfy a spectrum with a near ‘-5/3’ inertial subrange, suggesting its excellent capability for high Reynolds number atmospheric flows. It is more computationally efficient than other synthetic turbulence generation approaches, such as three-dimensional digital filter methods. A WRF-LES model with periodic boundary conditions was configured to provide a priori turbulent information for the synthetic turbulence generation method and used as an evaluation for the inflow case. The comparison shows that the inflow case generated similar turbulence structures as these in the periodic case after a short adjustment distance. The inflow case yielded a mean velocity profile in a good agreement with the desired one, and 2nd order moment statistics profiles close to the desired ones after a short distance. For the range of the integral length scale which we tested, its influence on the profiles of the mean velocities is not significant, whereas its influence on the second moment statistics profiles is evident, in particular for very small integral length scales. This implementation can be extended to the WRF-LES simulation of a horizontally inhomogeneous case with non-repeated surface landuse pattern and a multi-scale seamless nesting case from a meso-scale domain with a km-resolution down to LES domains with metre resolutions.
Exponential correlation function, Inflow turbulence generator, Large eddy simulation, atmospheric boundary layer
1991-9603
323-336
Zhong, Jian
23c5309f-425e-4fe9-b08e-1f67ea857427
Cai, Xiaoming
fec61328-e951-4caa-bcf2-3789e9ba6964
Xie, Zheng-Tong
98ced75d-5617-4c2d-b20f-7038c54f4ff0
Zhong, Jian
23c5309f-425e-4fe9-b08e-1f67ea857427
Cai, Xiaoming
fec61328-e951-4caa-bcf2-3789e9ba6964
Xie, Zheng-Tong
98ced75d-5617-4c2d-b20f-7038c54f4ff0

Zhong, Jian, Cai, Xiaoming and Xie, Zheng-Tong (2021) Implementation of a synthetic inflow turbulence generator in idealised WRF v3.6.1 large eddy simulations under neutral atmospheric conditions. Geoscientific Model Development, 14 (1), 323-336. (doi:10.5194/gmd-14-323-2021).

Record type: Article

Abstract

A synthetic inflow turbulence generator was implemented in the idealised Weather Research and Forecasting large eddy simulation (WRF-LES v3.6.1) model under neutral atmospheric conditions. This method is based on an exponential correlation function, and generates a series of two-dimensional slices of data which are correlated both in space and in time. These data satisfy a spectrum with a near ‘-5/3’ inertial subrange, suggesting its excellent capability for high Reynolds number atmospheric flows. It is more computationally efficient than other synthetic turbulence generation approaches, such as three-dimensional digital filter methods. A WRF-LES model with periodic boundary conditions was configured to provide a priori turbulent information for the synthetic turbulence generation method and used as an evaluation for the inflow case. The comparison shows that the inflow case generated similar turbulence structures as these in the periodic case after a short adjustment distance. The inflow case yielded a mean velocity profile in a good agreement with the desired one, and 2nd order moment statistics profiles close to the desired ones after a short distance. For the range of the integral length scale which we tested, its influence on the profiles of the mean velocities is not significant, whereas its influence on the second moment statistics profiles is evident, in particular for very small integral length scales. This implementation can be extended to the WRF-LES simulation of a horizontally inhomogeneous case with non-repeated surface landuse pattern and a multi-scale seamless nesting case from a meso-scale domain with a km-resolution down to LES domains with metre resolutions.

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More information

Submitted date: 24 June 2019
Accepted/In Press date: 19 July 2019
e-pub ahead of print date: 22 July 2019
Published date: 22 January 2021
Additional Information: Funding Information: This research has been supported by the UK Natural Environment Research Council (NERC) (grant no. NE/N003195/1). Publisher Copyright: © 2021 Author(s). This work is distributed under the Creative Commons Attribution 4.0 License.
Keywords: Exponential correlation function, Inflow turbulence generator, Large eddy simulation, atmospheric boundary layer

Identifiers

Local EPrints ID: 432872
URI: http://eprints.soton.ac.uk/id/eprint/432872
ISSN: 1991-9603
PURE UUID: 27b69bef-c5ec-45d6-8b29-f905f88acdbf
ORCID for Zheng-Tong Xie: ORCID iD orcid.org/0000-0002-8119-7532

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Date deposited: 31 Jul 2019 16:30
Last modified: 16 Mar 2024 03:40

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Contributors

Author: Jian Zhong
Author: Xiaoming Cai
Author: Zheng-Tong Xie ORCID iD

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