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Development of a new 1D urban canopy model: coherences between surface parameterizations

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Development of a new 1D urban canopy model: coherences between surface parameterizations

Graph Chatbot

Chattez avec Graph Search

How do patchy snow covers affect turbulent sensible heat fluxes? – Numerical analysis and experimental findings

A Modulated-Gradient Parametrization for the Large-Eddy Simulation of the Atmospheric Boundary Layer Using the Weather Research and Forecasting Model

Temperature statistics in the deep ocean

Wake flow in a wind farm during a diurnal cycle

Intercomparison of Terrain-Following Coordinate Transformation and Immersed Boundary Methods for Large-Eddy Simulation of Wind Fields over Complex Terrain

Theoretical and numerical studies of atmospheric boundary-layer flows over complex terrain

Influence of the Coriolis force on the structure and evolution of wind turbine wakes

Intercomparison of Terrain-Following Coordinate Transformation and Immersed Boundary Methods for Large-Eddy Simulation of Wind Fields over Complex Terrain

Counter-Gradient, Co-Gradient and ‘Surface-Layer' Momentum Fluxes in Nocturnal Slope Flows over Steep Alpine Terrain

Decoupling of mass flux and turbulent wind fluctuations in drifting snow

Temperature statistics in the deep ocean

How do patchy snow covers affect turbulent sensible heat fluxes? – Numerical analysis and experimental findings

Intercomparison of Terrain-Following Coordinate Transformation and Immersed Boundary Methods for Large-Eddy Simulation of Wind Fields over Complex Terrain

A Modulated-Gradient Parametrization for the Large-Eddy Simulation of the Atmospheric Boundary Layer Using the Weather Research and Forecasting Model

Wake flow in a wind farm during a diurnal cycle

Theoretical and numerical studies of atmospheric boundary-layer flows over complex terrain

Decoupling of mass flux and turbulent wind fluctuations in drifting snow

Influence of the Coriolis force on the structure and evolution of wind turbine wakes

Intercomparison of Terrain-Following Coordinate Transformation and Immersed Boundary Methods for Large-Eddy Simulation of Wind Fields over Complex Terrain

Counter-Gradient, Co-Gradient and ‘Surface-Layer' Momentum Fluxes in Nocturnal Slope Flows over Steep Alpine Terrain