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Marc Parlange

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Preferential Deposition of Snow and Dust Over Hills: Governing Processes and Relevant Scales

Large wind farms can destroy stratocumulus clouds-evidence from large eddy simulations.

Perturbations to the Spatial and Temporal Characteristics of the Diurnally-Varying Atmospheric Boundary Layer Due to an Extensive Wind Farm

Direct numberical simulation of turbulent slope flows up to Grash of number Gr=2.1 x 10(11)

Katabatic Flow: A Closed-Form Solution with Spatially-Varying Eddy Diffusivities

Spatial Characteristics of Roughness Sublayer Mean Flow and Turbulence Over a Realistic Urban Surface

Adapting tilt corrections and the governing flow equations for steep, fully three-dimensional, mountainous terrain

Attenuation of wind-induced pressure perturbations in alpine snow