Evaluating Terrain as a Turbulence Generation Method

When driving microscale large-eddy simulations with mesoscale model solutions, turbulence will take space to develop, known as <i>fetch</i>, on the microscale domain. To reduce fetch, it is common to add perturbations near the boundaries to speed up turbulence development. However, when...

Descripción completa

Guardado en:
Detalles Bibliográficos
Autores principales: Patrick Hawbecker, Matthew Churchfield
Formato: article
Lenguaje:EN
Publicado: MDPI AG 2021
Materias:
T
Acceso en línea:https://doaj.org/article/792122c919e345b9bda86e038d614c0d
Etiquetas: Agregar Etiqueta
Sin Etiquetas, Sea el primero en etiquetar este registro!
id oai:doaj.org-article:792122c919e345b9bda86e038d614c0d
record_format dspace
spelling oai:doaj.org-article:792122c919e345b9bda86e038d614c0d2021-11-11T15:43:19ZEvaluating Terrain as a Turbulence Generation Method10.3390/en142168581996-1073https://doaj.org/article/792122c919e345b9bda86e038d614c0d2021-10-01T00:00:00Zhttps://www.mdpi.com/1996-1073/14/21/6858https://doaj.org/toc/1996-1073When driving microscale large-eddy simulations with mesoscale model solutions, turbulence will take space to develop, known as <i>fetch</i>, on the microscale domain. To reduce fetch, it is common to add perturbations near the boundaries to speed up turbulence development. However, when simulating domains over complex terrain, it is possible that the terrain itself can quickly generate turbulence within the boundary layer. It is shown here that rugged terrain is able to generate turbulence without the assistance of a perturbation strategy; however, the levels of turbulence generated are improved when adding perturbations at the inlet. Flow over smoothed, but not flat, terrain fails to generate adequate turbulence throughout the boundary layer in all tests conducted herein. Sensitivities to the strength of the mean wind speed and boundary layer height are investigated and show that higher wind speeds produce turbulence over terrain features that slower wind speeds do not. Further, by increasing the height of the capping inversion, the effectiveness of topography alone to generate turbulence throughout the depth of the boundary is diminished. In all cases, the inclusion of a perturbation strategy improved simulation performance with respect to turbulence development.Patrick HawbeckerMatthew ChurchfieldMDPI AGarticleturbulenceterrainlarge-eddy simulationTechnologyTENEnergies, Vol 14, Iss 6858, p 6858 (2021)
institution DOAJ
collection DOAJ
language EN
topic turbulence
terrain
large-eddy simulation
Technology
T
spellingShingle turbulence
terrain
large-eddy simulation
Technology
T
Patrick Hawbecker
Matthew Churchfield
Evaluating Terrain as a Turbulence Generation Method
description When driving microscale large-eddy simulations with mesoscale model solutions, turbulence will take space to develop, known as <i>fetch</i>, on the microscale domain. To reduce fetch, it is common to add perturbations near the boundaries to speed up turbulence development. However, when simulating domains over complex terrain, it is possible that the terrain itself can quickly generate turbulence within the boundary layer. It is shown here that rugged terrain is able to generate turbulence without the assistance of a perturbation strategy; however, the levels of turbulence generated are improved when adding perturbations at the inlet. Flow over smoothed, but not flat, terrain fails to generate adequate turbulence throughout the boundary layer in all tests conducted herein. Sensitivities to the strength of the mean wind speed and boundary layer height are investigated and show that higher wind speeds produce turbulence over terrain features that slower wind speeds do not. Further, by increasing the height of the capping inversion, the effectiveness of topography alone to generate turbulence throughout the depth of the boundary is diminished. In all cases, the inclusion of a perturbation strategy improved simulation performance with respect to turbulence development.
format article
author Patrick Hawbecker
Matthew Churchfield
author_facet Patrick Hawbecker
Matthew Churchfield
author_sort Patrick Hawbecker
title Evaluating Terrain as a Turbulence Generation Method
title_short Evaluating Terrain as a Turbulence Generation Method
title_full Evaluating Terrain as a Turbulence Generation Method
title_fullStr Evaluating Terrain as a Turbulence Generation Method
title_full_unstemmed Evaluating Terrain as a Turbulence Generation Method
title_sort evaluating terrain as a turbulence generation method
publisher MDPI AG
publishDate 2021
url https://doaj.org/article/792122c919e345b9bda86e038d614c0d
work_keys_str_mv AT patrickhawbecker evaluatingterrainasaturbulencegenerationmethod
AT matthewchurchfield evaluatingterrainasaturbulencegenerationmethod
_version_ 1718434093104889856