WRF-LES Simulation of the Boundary Layer Turbulent Processes during the BLLAST Campaign

A real case long-term nested large eddy simulation (LES) of 25-day duration is performed using the WRF-LES modelling system, with a maximum horizontal grid resolution of 111 m, in order to explore the ability of the model to reproduce the turbulence magnitudes within the first tens of metres of the...

Full description

Bibliographic Details
Main Authors: Mireia Udina, Àlex Montornès, Pau Casso, Branko Kosović, Joan Bech
Format: Article
Language:English
Published: MDPI AG 2020-10-01
Series:Atmosphere
Subjects:
WRF
Online Access:https://www.mdpi.com/2073-4433/11/11/1149
id doaj-a061096a4eaf472c857e97d45f7e6f4f
record_format Article
spelling doaj-a061096a4eaf472c857e97d45f7e6f4f2020-11-25T03:09:37ZengMDPI AGAtmosphere2073-44332020-10-01111149114910.3390/atmos11111149WRF-LES Simulation of the Boundary Layer Turbulent Processes during the BLLAST CampaignMireia Udina0Àlex Montornès1Pau Casso2Branko Kosović3Joan Bech4Departament de Física Aplicada-Meteorologia, Universitat de Barcelona, C/ Martí i Franquès, 1, 08028 Barcelona, SpainVORTEX, 08042 Barcelona, SpainVORTEX, 08042 Barcelona, SpainNational Center for Atmospheric Research, Boulder, CO 80307, USADepartament de Física Aplicada-Meteorologia, Universitat de Barcelona, C/ Martí i Franquès, 1, 08028 Barcelona, SpainA real case long-term nested large eddy simulation (LES) of 25-day duration is performed using the WRF-LES modelling system, with a maximum horizontal grid resolution of 111 m, in order to explore the ability of the model to reproduce the turbulence magnitudes within the first tens of metres of the boundary layer. Sonic anemometer measurements from a 60-m tower installed during the Boundary Layer Late Afternoon and Sunset Turbulence (BLLAST) field campaign are used for verification, which is focused on the turbulent magnitudes in order to assess the success and limitations in resolving turbulent flow characteristics. The mesoscale and LES simulations reproduce the wind speed and direction fairly well, but only LES is able to reproduce the energy of eddies with lifetimes shorter than a few hours. The turbulent kinetic energy in LES simulation is generally underestimated during the daytime, mainly due to a vertical velocity standard deviation that is too low. The turbulent heat flux is misrepresented in the model, probably due to the inaccuracy of the sub-grid scheme.https://www.mdpi.com/2073-4433/11/11/1149large eddy simulationverificationturbulenceWRF
collection DOAJ
language English
format Article
sources DOAJ
author Mireia Udina
Àlex Montornès
Pau Casso
Branko Kosović
Joan Bech
spellingShingle Mireia Udina
Àlex Montornès
Pau Casso
Branko Kosović
Joan Bech
WRF-LES Simulation of the Boundary Layer Turbulent Processes during the BLLAST Campaign
Atmosphere
large eddy simulation
verification
turbulence
WRF
author_facet Mireia Udina
Àlex Montornès
Pau Casso
Branko Kosović
Joan Bech
author_sort Mireia Udina
title WRF-LES Simulation of the Boundary Layer Turbulent Processes during the BLLAST Campaign
title_short WRF-LES Simulation of the Boundary Layer Turbulent Processes during the BLLAST Campaign
title_full WRF-LES Simulation of the Boundary Layer Turbulent Processes during the BLLAST Campaign
title_fullStr WRF-LES Simulation of the Boundary Layer Turbulent Processes during the BLLAST Campaign
title_full_unstemmed WRF-LES Simulation of the Boundary Layer Turbulent Processes during the BLLAST Campaign
title_sort wrf-les simulation of the boundary layer turbulent processes during the bllast campaign
publisher MDPI AG
series Atmosphere
issn 2073-4433
publishDate 2020-10-01
description A real case long-term nested large eddy simulation (LES) of 25-day duration is performed using the WRF-LES modelling system, with a maximum horizontal grid resolution of 111 m, in order to explore the ability of the model to reproduce the turbulence magnitudes within the first tens of metres of the boundary layer. Sonic anemometer measurements from a 60-m tower installed during the Boundary Layer Late Afternoon and Sunset Turbulence (BLLAST) field campaign are used for verification, which is focused on the turbulent magnitudes in order to assess the success and limitations in resolving turbulent flow characteristics. The mesoscale and LES simulations reproduce the wind speed and direction fairly well, but only LES is able to reproduce the energy of eddies with lifetimes shorter than a few hours. The turbulent kinetic energy in LES simulation is generally underestimated during the daytime, mainly due to a vertical velocity standard deviation that is too low. The turbulent heat flux is misrepresented in the model, probably due to the inaccuracy of the sub-grid scheme.
topic large eddy simulation
verification
turbulence
WRF
url https://www.mdpi.com/2073-4433/11/11/1149
work_keys_str_mv AT mireiaudina wrflessimulationoftheboundarylayerturbulentprocessesduringthebllastcampaign
AT alexmontornes wrflessimulationoftheboundarylayerturbulentprocessesduringthebllastcampaign
AT paucasso wrflessimulationoftheboundarylayerturbulentprocessesduringthebllastcampaign
AT brankokosovic wrflessimulationoftheboundarylayerturbulentprocessesduringthebllastcampaign
AT joanbech wrflessimulationoftheboundarylayerturbulentprocessesduringthebllastcampaign
_version_ 1724661448389427200