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ENVIRONMENTAL FLUID MECHANICS
Journal
Identifier:
E058759
ISSN:
1567-7419
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A dry deposition scheme for particulate matter coupled with a well-known Lagrangian Stochastic model for pollutant dispersion
Academic Article
A minimal model of adiabatic isotherms surfacing in very shallow waters
Academic Article
A multimedia chemical fate model with time-dependent air-water transfer rates.
Academic Article
A stochastic Lagrangian micromixing model for the dispersion of reactive scalars in turbulent flows: role of concentration fluctuations and improvements to the conserved scalar theory under non-homogeneous conditions
Academic Article
An analytical solution of the advection-diffusion equation considering non-local turbulence closure
Academic Article
Analytical evaluation of mesoscale fluxes and pressure field.
Academic Article
Atmospheric mercury at mediterranean coastal stations.
Academic Article
Comparison of atmospheric modelling systems simulating the flow, turbulence and dispersion at the microscale within obstacles
Academic Article
Entropic approach to estimate the mean flow velocity: experimental investigation in laboratory flumes
Academic Article
Evaluation of the Atmospheric RAMS Model in an Obstacle Resolving Configuration.
Academic Article
Intercomparison of two models, ETA and RAMS, with TRACT field campaign data
Academic Article
Modeling mercury emissions from forest fires in the Mediterranean region
Academic Article
Numerical experiments with RAMS model in highly complex terrain
Academic Article
Spatial and temporal distribution of atmospheric mercury species over the Adriatic Sea.
Academic Article
Statistical properties of concentration fluctuations in two merging plumes
Academic Article
Strong solutions for Richards' equation with Cauchy conditions and constant pressure gradient
Academic Article
Turbulence closure models and their application in RAMS
Academic Article
Turbulence closure models and their application in RAMS
Academic Article
Turbulence perturbations in the neutrally stratified surface layer due to interaction of katabatic flow with a steep ridge.
Academic Article
Turbulence perturbations in the neutrally stratified surface layer due to the interaction of a katabatic flow with a steep ridge
Academic Article
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