A nested multi-scale system implemented in the large-eddy simulation model PALM model system 6.0

<p>Large-eddy simulation (LES) provides a physically sound approach to study complex turbulent processes within the atmospheric boundary layer including urban boundary layer flows. However, such flow problems often involve a large separation of turbulent scales, requiring a large computational...

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Main Authors: A. Hellsten, K. Ketelsen, M. Sühring, M. Auvinen, B. Maronga, C. Knigge, F. Barmpas, G. Tsegas, N. Moussiopoulos, S. Raasch
Format: Article
Language:English
Published: Copernicus Publications 2021-06-01
Series:Geoscientific Model Development
Online Access:https://gmd.copernicus.org/articles/14/3185/2021/gmd-14-3185-2021.pdf
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spelling doaj-6d6329ec44ba4557bf4fd19d9f5bd0302021-06-03T07:20:09ZengCopernicus PublicationsGeoscientific Model Development1991-959X1991-96032021-06-01143185321410.5194/gmd-14-3185-2021A nested multi-scale system implemented in the large-eddy simulation model PALM model system 6.0A. Hellsten0K. Ketelsen1M. Sühring2M. Auvinen3B. Maronga4B. Maronga5C. Knigge6F. Barmpas7G. Tsegas8N. Moussiopoulos9S. Raasch10Finnish Meteorological Institute, P.O. Box 503, 00101, Helsinki, FinlandSoftware Consultant, Beethovenstr. 29A, 12247 Berlin, GermanyLeibniz University Hannover, Institute of Meteorology and Climatology, Herrenhäuser Strasse 2, 30419 Hanover, GermanyFinnish Meteorological Institute, P.O. Box 503, 00101, Helsinki, FinlandLeibniz University Hannover, Institute of Meteorology and Climatology, Herrenhäuser Strasse 2, 30419 Hanover, GermanyUniversity of Bergen, Geophysical Institute, Postboks 7803, 5020 Bergen, NorwayDeutscher Wetterdienst, Frankfurter Straße 135, 63067 Offenbach, GermanyAristotle University Thessaloniki, P.O. Box 483, 54124, Thessaloniki, GreeceAristotle University Thessaloniki, P.O. Box 483, 54124, Thessaloniki, GreeceAristotle University Thessaloniki, P.O. Box 483, 54124, Thessaloniki, GreeceLeibniz University Hannover, Institute of Meteorology and Climatology, Herrenhäuser Strasse 2, 30419 Hanover, Germany<p>Large-eddy simulation (LES) provides a physically sound approach to study complex turbulent processes within the atmospheric boundary layer including urban boundary layer flows. However, such flow problems often involve a large separation of turbulent scales, requiring a large computational domain and very high grid resolution near the surface features, leading to prohibitive computational costs. To overcome this problem, an online LES–LES nesting scheme is implemented into the PALM model system 6.0. The hereby documented and evaluated nesting method is capable of supporting multiple child domains, which can be nested within their parent domain either in a parallel or recursively cascading configuration. The nesting system is evaluated by first simulating a purely convective boundary layer flow system and then three different neutrally stratified flow scenarios with increasing order of topographic complexity. The results of the nested runs are compared with corresponding non-nested high- and low-resolution results. The results reveal that the solution accuracy within the high-resolution nest domain is clearly improved as the solutions approach the non-nested high-resolution reference results. In obstacle-resolving LES, the two-way coupling becomes problematic as anterpolation introduces a regional discrepancy within the obstacle canopy of the parent domain. This is remedied by introducing canopy-restricted anterpolation where the operation is only performed above the obstacle canopy. The test simulations make evident that this approach is the most suitable coupling strategy for obstacle-resolving LES. The performed simulations testify that nesting can reduce the CPU time up to 80 % compared to the fine-resolution reference runs, while the computational overhead from the nesting operations remained below 16 % for the two-way coupling approach and significantly less for the one-way alternative.</p>https://gmd.copernicus.org/articles/14/3185/2021/gmd-14-3185-2021.pdf
collection DOAJ
language English
format Article
sources DOAJ
author A. Hellsten
K. Ketelsen
M. Sühring
M. Auvinen
B. Maronga
B. Maronga
C. Knigge
F. Barmpas
G. Tsegas
N. Moussiopoulos
S. Raasch
spellingShingle A. Hellsten
K. Ketelsen
M. Sühring
M. Auvinen
B. Maronga
B. Maronga
C. Knigge
F. Barmpas
G. Tsegas
N. Moussiopoulos
S. Raasch
A nested multi-scale system implemented in the large-eddy simulation model PALM model system 6.0
Geoscientific Model Development
author_facet A. Hellsten
K. Ketelsen
M. Sühring
M. Auvinen
B. Maronga
B. Maronga
C. Knigge
F. Barmpas
G. Tsegas
N. Moussiopoulos
S. Raasch
author_sort A. Hellsten
title A nested multi-scale system implemented in the large-eddy simulation model PALM model system 6.0
title_short A nested multi-scale system implemented in the large-eddy simulation model PALM model system 6.0
title_full A nested multi-scale system implemented in the large-eddy simulation model PALM model system 6.0
title_fullStr A nested multi-scale system implemented in the large-eddy simulation model PALM model system 6.0
title_full_unstemmed A nested multi-scale system implemented in the large-eddy simulation model PALM model system 6.0
title_sort nested multi-scale system implemented in the large-eddy simulation model palm model system 6.0
publisher Copernicus Publications
series Geoscientific Model Development
issn 1991-959X
1991-9603
publishDate 2021-06-01
description <p>Large-eddy simulation (LES) provides a physically sound approach to study complex turbulent processes within the atmospheric boundary layer including urban boundary layer flows. However, such flow problems often involve a large separation of turbulent scales, requiring a large computational domain and very high grid resolution near the surface features, leading to prohibitive computational costs. To overcome this problem, an online LES–LES nesting scheme is implemented into the PALM model system 6.0. The hereby documented and evaluated nesting method is capable of supporting multiple child domains, which can be nested within their parent domain either in a parallel or recursively cascading configuration. The nesting system is evaluated by first simulating a purely convective boundary layer flow system and then three different neutrally stratified flow scenarios with increasing order of topographic complexity. The results of the nested runs are compared with corresponding non-nested high- and low-resolution results. The results reveal that the solution accuracy within the high-resolution nest domain is clearly improved as the solutions approach the non-nested high-resolution reference results. In obstacle-resolving LES, the two-way coupling becomes problematic as anterpolation introduces a regional discrepancy within the obstacle canopy of the parent domain. This is remedied by introducing canopy-restricted anterpolation where the operation is only performed above the obstacle canopy. The test simulations make evident that this approach is the most suitable coupling strategy for obstacle-resolving LES. The performed simulations testify that nesting can reduce the CPU time up to 80 % compared to the fine-resolution reference runs, while the computational overhead from the nesting operations remained below 16 % for the two-way coupling approach and significantly less for the one-way alternative.</p>
url https://gmd.copernicus.org/articles/14/3185/2021/gmd-14-3185-2021.pdf
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