Search results for "Roughness length"

showing 9 items of 9 documents

The effect of the slope of irregularly distributed roughness elements on turbulent wall-bounded flows

2008

Wall roughness produces a downward shift of the mean streamwise velocity profile in the log region, known as the roughness function. The dependence of the roughness function on the height and arrangement of roughness elements has been confirmed in several studies where regular rough walls were analysed; less attention has been paid to non-regular rough walls. Here, a numerical analysis of turbulent flows over irregularly shaped rough walls is performed, clearly identifying the importance of a parameter, called the effective slope (ES) of the wall corrugations, in characterizing the geometry of non-smooth irregular walls. The effective slope proves to be one of the fundamental geometric para…

Physicsbusiness.industryTurbulenceMechanical Engineeringturbulencelarge eddy simulationGeometrySurface finishCondensed Matter PhysicsSettore ICAR/01 - Idraulicawall roughness; turbulence; large eddy simulationOpticsRoughness lengthwall roughnessMechanics of MaterialsParasitic dragDragRough-wall turbulent flow LESSurface roughnessRange (statistics)businesswall roughneScaling
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Effects of irregular two-dimensional and three-dimensional surface roughness in turbulent channel flows

2012

Abstract Wall-resolved Large Eddy Simulation of fully developed turbulent channel flows over two different rough surfaces is performed to investigate on the effects of irregular 2D and 3D roughness on the turbulence. The two geometries are obtained through the superimposition of sinusoidal functions having random amplitudes and different wave lengths. In the 2D configuration the irregular shape in the longitudinal direction is replicated in the transverse one, while in the 3D case the sinusoidal functions are generated both in streamwise and spanwise directions. Both channel walls are roughened in such a way as to obtain surfaces with statistically equivalent roughness height, but different…

Fluid Flow and Transfer ProcessesMaterials scienceTurbulencebusiness.industryMechanical EngineeringReynolds numberGeometrySurface finishReynolds stressCondensed Matter PhysicsOpen-channel flowSettore ICAR/01 - IdraulicaPhysics::Fluid DynamicsTurbulencesymbols.namesakeOpticsRoughness lengthLarge Eddy simulationSurface roughnesssymbolsRoughnebusinessLarge eddy simulation
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Improving RAMS and WRF mesoscale forecasts over two distinct vegetation covers using an appropriate thermal roughness length parameterization

2019

Land Surface Models (LSM) have shown some difficulties to properly simulate day-time 2-m air and surface skin temperatures. This kind of models are coupled to atmospheric models in mesoscale modelling, such as the Regional Atmospheric Modeling System (RAMS) and the Weather Research and Forecasting (WRF) Model. This model coupling is used within Numerical Weather Prediction Systems (NWP) in order to forecast key physical processes for agricultural meteorology and forestry as well as in ecological modelling. The current study first evaluates the surface energy fluxes and temperatures simulated by these two state-of-the-art NWP models over two distinct vegetated covers, one corresponding to a …

Atmospheric ScienceGlobal and Planetary ChangeMeteorologyNumerical weather prediction/forecastingFísica de la TierraMesoscale meteorologyEuropean Regional Development FundSurface-layer parameterizationForestryVegetationMesoscale modellingBoscos i silviculturaSurface energy fluxRoughness lengthThermal roughness lengthWeather Research and Forecasting ModelEnvironmental scienceLand surface modelsSurface energy fluxesAgronomy and Crop SciencePhysics::Atmospheric and Oceanic Physics
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Numerical Modelling of the Urban Climate

1988

Three-dimensional numerical models of the urban climate have been developed in order to simulate climatic changes and air pollution in urban regions due to anthropogenic activities. Two versions are presented. Model A covers mesoscale γ and uses the roughness length to characterize surface structure. The microscale version B approximates the actual urban build-up by rectangular blocks. Model A results agree reasonably well with observations. For complex building structures, the microscale model must be applied. Model B results on neutral flow and pollutant transport within a particular building configuration are discussed.

GeographyRoughness lengthMeteorologyUrban climateFlow (psychology)Air pollutionmedicinePollutant transportMesoscale meteorologySurface structuremedicine.disease_causeMicroscale chemistry
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Impact of very low crop residues cover on wind erosion in the Sahel

2011

International audience; In the Sahel, with average annual precipitation in the order of 500 mm yr− 1, wind erosion occurs mainly on cultivated millet fields whose surfaces are only partially covered by crop residues. The impact of these residues on wind erosion was not clearly established. The objective of this study is thus to quantify the actual amount of crop residues in traditional Sahelian fields and to determine their impacts on wind erosion by reference to a bare surface throughout the seasonal cycle over several years. At the beginning of the year during dry season, Sahelian farmers use to "clean" their fields, i.e. cut and lay flat on the soil surface any millet stalks still standi…

Wet seasonCrop residuecrop residuescover010504 meteorology & atmospheric sciencesAGROCLIMATOLOGIE[SDE.MCG]Environmental Sciences/Global ChangesCrop residues coverSoil surface01 natural sciencesEROSION EOLIENNEcrop residue coverDry season[ SDU.ENVI ] Sciences of the Universe [physics]/Continental interfaces environmentClearingPrecipitationNigerwind erosion[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment0105 earth and related environmental sciencesEarth-Surface Processesmillet field2. Zero hungerHydrologyRESIDU VEGETAL04 agricultural and veterinary sciences15. Life on landAerodynamic roughness length[ SDE.MCG ] Environmental Sciences/Global ChangesMillet fieldAgronomyWind erosion040103 agronomy & agricultureErosion0401 agriculture forestry and fisheriesEnvironmental scienceAeolian processesAerodynamic roughness
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Turbulence structures over irregular rough surfaces

2010

Turbulent flow in a channel with irregular two-dimensional rough surfaces is analysed through wall-resolving large eddy simulation (LES). Both walls of the channel are roughened through the superimposition of sinusoidal functions having random amplitude and four different wavelengths. The downward shift of the velocity profile in the log region due to the roughness, known as roughness function, is well captured in the simulations. The spanwise and wall-normal turbulence intensities are found to increase with the roughness height, while the streamwise component decreases. The analysis of the Reynolds stress anisotropy tensor highlights a tendency towards isotropisation, confirmed by the vort…

Materials scienceComputational MechanicsGeneral Physics and Astronomyturbulence; irregular rough wall; LESSurface finishReynolds stresschannel flowSettore ICAR/01 - IdraulicaPhysics::Fluid Dynamicsirregular rough wallOpticsirregular roughneAnisotropyturbulence structureTurbulencebusiness.industryturbulenceMechanicsVorticityCondensed Matter PhysicsOpen-channel flowRoughness lengthMechanics of MaterialsLESbusinessLarge eddy simulation
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Estimation of annual energy output of a wind turbine using wind speed probability distribution

2016

In this work, annual energy output of a variable speed wind turbine is analyzed using annual Weibull wind speed probability distribution function. The power coefficient variation with tip speed ratio in torque control region as well as pitch angle variation for maximum power output from wind turbine are analyzed for identifying control system parameters. The wind turbine power output and variation of power coefficient with tip speed ratio as well as pitch angle are examined / reported using annual Weibull distribution function. Finally the variation of the estimated annual energy output of the given wind turbine with the mean wind speed is presented.

Tip-speed ratioEngineeringWind gradientWind powerMeteorologybusiness.industry020209 energy02 engineering and technologyWind speedVariable speed wind turbineRoughness lengthWind profile power lawLog wind profileControl theoryPhysics::Space Physics0202 electrical engineering electronic engineering information engineeringbusinessPhysics::Atmospheric and Oceanic Physics2016 3rd International Conference on Electrical Energy Systems (ICEES)
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A sensitivity analysis of a surface energy balance model to LAI (Leaf Area Index)

2008

The LAI is a key parameter in hydrological processes, especially in the physically based distribution models. It is a critical ecosystem attribute since physiological processes such as photosynthesis, transpiration and evaporation depend on it. The diffusion of water vapor, momentum, heat and light through the canopy is regulated by the distribution and density of the leaves, branches, twigs and stems. The LAI influences the sensible heat flux H in the surface energy balance single source models through the calculation of the roughness length and of the displacement height. The aerodynamic resistance between the soil and within-canopy source height is a function of the LAI through the rough…

CanopyGeographyRoughness lengthSurface energy balance LAIMeteorologyHeat fluxEnergy balanceDiffusion (business)Leaf area indexSensible heatAtmospheric sciencesTranspirationSPIE Proceedings
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The making of the New European Wind Atlas - Part 1: Model sensitivity

2020

This is the first of two papers that document the creation of the New European Wind Atlas (NEWA). It describes the sensitivity analysis and evaluation procedures that formed the basis for choosing the final setup of the mesoscale model simulations of the wind atlas. The suitable combination of model setup and parameterizations, bound by practical constraints, was found for simulating the climatology of the wind field at turbine-relevant heights with the Weather Research and Forecasting (WRF) model. Initial WRF model sensitivity experiments compared the wind climate generated by using two commonly used planetary boundary layer schemes and were carried out over several regions in Europe. They…

010504 meteorology & atmospheric sciencesMeteorologyPlanetary boundary layer010505 oceanography020209 energylcsh:QE1-996.5Mesoscale meteorologyFísica atmosférica02 engineering and technology01 natural sciences7. Clean energyWind speedlcsh:GeologyBoundary layerRoughness length/dk/atira/pure/sustainabledevelopmentgoals/climate_action13. Climate actionWeather Research and Forecasting ModelWind resource assessmentWind atlasSDG 13 - Climate Action0202 electrical engineering electronic engineering information engineeringEnvironmental science0105 earth and related environmental sciences
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