Mixing and dissipation in particle-driven gravity currents
By F. Necker, C. Härtel, L. Kleiser, Eckart Meiburg. Journal of Fluid Mechanics, 2005
198 citations recorded by the source corpus.
Subfields: Computational Mechanics, Earth-Surface Processes, Ocean Engineering
View Paper: https://www.semanticscholar.org/paper/c42e854968d05cdb23eb49d4d9e560685ad41feb
How researchers see this paper
The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.
In Computational Mechanics
- Ben Kneller
- Eckart Meiburg
- S. Balachandar
- L. Weber
- Seng Keat Ooi
- G. Constantinescu
- Mariano I. Cantero
- Marcelo H. García
In Earth-Surface Processes
- Ben Kneller
- Eckart Meiburg
- S. Balachandar
- Mariano I. Cantero
- Marcelo H. García
- J. R. Lee
- L. Weber
- Seng Keat Ooi
In Ocean Engineering
- Ben Kneller
- Eckart Meiburg
- S. Balachandar
- Mariano I. Cantero
- Marcelo H. García
- J. R. Lee
- G. Constantinescu
- Detlef Lohse
Citations in the corpus
- Turbidity Currents and Their Deposits (2010, background): “In a follow-up study, Necker et al. (2005) analyzed the differences between shallow- and deepwater flows with regard to the energy budgets and mixing behavior.”
- On the front velocity of gravity currents (2007, methodology): “…gravity current’s front and the maximum spreading distance has motivated the development of relatively simple models (Allen 1985) all the way to detailed simulations (Lee & Wilhelmson 1997a , b; Härtel, Meiburg & Necker 2000b; Necker et al. 2002, 2005; Özgökmen et al. 2004; Cantero et al. 2006).”
- Numerical simulations of lock-exchange compositional gravity current (2009, background): “(6) Following Necker et al. (2005), in the case of compositional currents a differential equation relating the rates of change of the potential and kinetic energies can be obtained if the velocity components are assumed to be equal to zero on all the non-periodic boundaries and if the effects of dif”