Shear instability and coherent structures in shallow flow adjacent to a porous layer
By B. White, H. Nepf. Journal of Fluid Mechanics, 2007
302 citations recorded by the source corpus.
Subfields: Earth-Surface Processes, Ecology, Global and Planetary Change
View Paper: https://www.semanticscholar.org/paper/a99a1780ea44c9be7cbe36801e280850a018bba2
How researchers see this paper
The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.
In Earth-Surface Processes
In Ecology
In Global and Planetary Change
- H. Nepf
- R. Shaw
- E. Patton
- J. Finnigan
- Gabriel G. Katul
- Dennis D. Baldocchi
- Vladimir Nikora
- A. Sogachev
Citations in the corpus
- Turbulence structure above a vegetation canopy (2009, methodology): “We note also that the measurements of Ghisalberti & Nepf (2002) in a quasi-two-dimensional shallow-water flow over a canopy and those of White & Nepf (2007) in a truly two-dimensional canopy flow had transverse vortex wavelengths that matched the primary Kelvin– Helmholtz value of λ ∼= 7.0δω rather…”
- The wake structure behind a porous obstruction and its implications for deposition near a finite patch of emergent vegetation (2012, background): “Because the velocity continues to decelerate and diverge for a short distance after the patch, the exit velocity (Ue) is slightly larger than the steady wake velocity (U1).”
- The terms of turbulent kinetic energy budget within random arrays of emergent cylinders (2014, unknown): “These combined with analytical [Negretti et al., 2006] and laboratory studies at this scale [Nepf, 1999; White and Nepf, 2003, 2007; Ferreira et al., 2009] have mostly advanced the knowledge on fluxes of mass and momentum, for instance, clarifying the nature of turbulent and dispersive stresses.”