An Intercomparison of LES Subgrid-Scale Models for Simulations of Slope Flows

We propose an inter-comparison of Smagorinsky type subgrid-scale models for the simulation of high Reynolds number katabatic flows, with the purpose of testing the validity of some of the model's assumptions for the considered application. Katabatic flows arise along sloping surfaces under stab...

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Main Authors: Giometto, Marco Giovanni, Parlange, Marc, Fang, Jiannong
Format: Text
Language:unknown
Published: 2015
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Online Access:http://infoscience.epfl.ch/record/206720
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spelling ftinfoscience:oai:infoscience.tind.io:206720 2023-05-15T13:48:06+02:00 An Intercomparison of LES Subgrid-Scale Models for Simulations of Slope Flows Giometto, Marco Giovanni Parlange, Marc Fang, Jiannong 2015-03-16T11:26:02Z http://infoscience.epfl.ch/record/206720 unknown http://infoscience.epfl.ch/record/206720 http://infoscience.epfl.ch/record/206720 Text 2015 ftinfoscience 2023-02-13T22:25:57Z We propose an inter-comparison of Smagorinsky type subgrid-scale models for the simulation of high Reynolds number katabatic flows, with the purpose of testing the validity of some of the model's assumptions for the considered application. Katabatic flows arise along sloping surfaces under stably stratified conditions and are a direct consequence of surface cooling. Understanding their structure is of great interest in meteorology because of the broad band of areas and scales that they cover, influencing from local valleys microclimate (e.g. over Salt Lake and Phoenix valleys) to synoptic scale motions (e.g. over Antarctica). Large-eddy simulation (LES), on the other hand, represents an important tool to study high-Reynolds number flows and has undergone significant developments and validations in the past years, confirming its reliability when adopted to simulate a variety of atmospheric (and industrial) flows. The stable stratification of the environment and the complex dynamics that arise close to the surface in katabatic winds – leading eventually to the formation of the so-called low level jet – represent a tough test case for closure models, questioning their applicability over a broad range of filter (grid) scales and motivating the proposed work. The study is performed in the idealized framework of the Prandtl model, the set of normalized, filtered Boussinesq equations is solved on a regular domain, adopting an in-house mixed pseudo-spectral / finite difference code. The original static Smagorinsky model (SMAG), the standard dynamic model with planar averaging of the coefficient (PASI) and the more recent scale-dependent Smagorinsky model with Lagrangian averaging of the coefficients (LASD) are adopted to independently parametrize the subgrid-scale terms for kinematic momentum and energy, which arise from the filtering operation. Results focus on the statistically steady state solution of the problem and show how mean profiles are consistent across subgrid-scale models and most of the discretizations, ... Text Antarc* Antarctica EPFL Infoscience (Ecole Polytechnique Fédérale Lausanne)
institution Open Polar
collection EPFL Infoscience (Ecole Polytechnique Fédérale Lausanne)
op_collection_id ftinfoscience
language unknown
description We propose an inter-comparison of Smagorinsky type subgrid-scale models for the simulation of high Reynolds number katabatic flows, with the purpose of testing the validity of some of the model's assumptions for the considered application. Katabatic flows arise along sloping surfaces under stably stratified conditions and are a direct consequence of surface cooling. Understanding their structure is of great interest in meteorology because of the broad band of areas and scales that they cover, influencing from local valleys microclimate (e.g. over Salt Lake and Phoenix valleys) to synoptic scale motions (e.g. over Antarctica). Large-eddy simulation (LES), on the other hand, represents an important tool to study high-Reynolds number flows and has undergone significant developments and validations in the past years, confirming its reliability when adopted to simulate a variety of atmospheric (and industrial) flows. The stable stratification of the environment and the complex dynamics that arise close to the surface in katabatic winds – leading eventually to the formation of the so-called low level jet – represent a tough test case for closure models, questioning their applicability over a broad range of filter (grid) scales and motivating the proposed work. The study is performed in the idealized framework of the Prandtl model, the set of normalized, filtered Boussinesq equations is solved on a regular domain, adopting an in-house mixed pseudo-spectral / finite difference code. The original static Smagorinsky model (SMAG), the standard dynamic model with planar averaging of the coefficient (PASI) and the more recent scale-dependent Smagorinsky model with Lagrangian averaging of the coefficients (LASD) are adopted to independently parametrize the subgrid-scale terms for kinematic momentum and energy, which arise from the filtering operation. Results focus on the statistically steady state solution of the problem and show how mean profiles are consistent across subgrid-scale models and most of the discretizations, ...
format Text
author Giometto, Marco Giovanni
Parlange, Marc
Fang, Jiannong
spellingShingle Giometto, Marco Giovanni
Parlange, Marc
Fang, Jiannong
An Intercomparison of LES Subgrid-Scale Models for Simulations of Slope Flows
author_facet Giometto, Marco Giovanni
Parlange, Marc
Fang, Jiannong
author_sort Giometto, Marco Giovanni
title An Intercomparison of LES Subgrid-Scale Models for Simulations of Slope Flows
title_short An Intercomparison of LES Subgrid-Scale Models for Simulations of Slope Flows
title_full An Intercomparison of LES Subgrid-Scale Models for Simulations of Slope Flows
title_fullStr An Intercomparison of LES Subgrid-Scale Models for Simulations of Slope Flows
title_full_unstemmed An Intercomparison of LES Subgrid-Scale Models for Simulations of Slope Flows
title_sort intercomparison of les subgrid-scale models for simulations of slope flows
publishDate 2015
url http://infoscience.epfl.ch/record/206720
genre Antarc*
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genre_facet Antarc*
Antarctica
op_source http://infoscience.epfl.ch/record/206720
op_relation http://infoscience.epfl.ch/record/206720
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