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David R. Fuhrman

Researcher at Technical University of Denmark

Publications -  121
Citations -  3877

David R. Fuhrman is an academic researcher from Technical University of Denmark. The author has contributed to research in topics: Turbulence & Breaking wave. The author has an hindex of 29, co-authored 103 publications receiving 2979 citations. Previous affiliations of David R. Fuhrman include DHI Water & Environment & University of Copenhagen.

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Numerical simulation of tsunami-scale wave boundary layers

TL;DR: In this paper, an existing 1DV boundary layer model, based on the horizontal component of the incompressible Reynolds-averaged Navier-Stokes (RANS) equations, is newly extended to incorporate a transitional variant of the standard two-equation k-ω turbulence closure.
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A numerical study of crescent waves

TL;DR: In this paper, a high-order Boussinesq model is used to conduct a systematic numerical study of crescent (or horseshoe) water wave patterns in a tank, arising from the instability of steep deep-water waves to 3D disturbances.
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Experimental study of tsunami-induced scour around a monopile foundation

TL;DR: In this article, the authors present an experimental study of the tsunami-induced scour process around a monopile foundation, representative of those commonly used for offshore wind farms, by subjecting the monopile to a time varying current, which enables a properly downscaled experiment from the boundary layer and scour perspective.
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Surf similarity and solitary wave runup

TL;DR: In this paper, the surf similarity parameter for solitary waves is reduced to the beach slope divided by the offshore wave height to depth ratio, which is defined as the ratio between the wave height and depth ratio.
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Bed slope effects on turbulent wave boundary layers: 1. Model validation and quantification of rough‐turbulent results

TL;DR: In this paper, a numerical model solving incompressible Reynolds-averaged Navier-Stokes equations, combined with a two-equation k-ω turbulence closure, is used to study converging-diverging effects from a sloping bed on turbulent (oscillatory) wave boundary layers.