A comprehensive numerical model of steady state saltation (COMSALT)
By J. Kok, Nilton O. Renno. 2009
308 citations recorded by the source corpus.
Subfields: Earth-Surface Processes, Ocean Engineering, Soil Science
View Paper: https://www.semanticscholar.org/paper/16900113548839fb8c400eae32534ccbb2519bc2
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
- Orencio Durán
- J. Kok
- Bruno Andreotti
- Thomas Pahtz
- Abram H. Clark
- Manousos Valyrakis
- P. Claudin
- M. Mikami
In Ocean Engineering
- Orencio Durán
- Bruno Andreotti
- J. Kok
- P. Claudin
- Thomas Pahtz
- Manousos Valyrakis
- Abram H. Clark
- G. Fratini
In Soil Science
- J. Kok
- Orencio Durán
- Thomas Pahtz
- Abram H. Clark
- Manousos Valyrakis
- P. Claudin
- Bruno Andreotti
- Olivier Pouliquen
Citations in the corpus
- On aeolian transport: Grain-scale interactions, dynamical mechanisms and scaling laws (2011, background): “…(1964), Anderson and Hallet (1986), Anderson and Haff (1988, 1991), Werner (1990), McEwan and Willetts (1991, 1993), Rasmussen and Sorensen (2008), Kok and Renno (2009), and Creyssels et al. (2009) – among others – have solved a simplified hydrodynamic model that neglects the turbulent…”
- Numerical simulation of turbulent sediment transport, from bed load to saltation (2011, methodology): “To avoid these issues, we use here a discrete element method for the particles [20, 21, 62–64].”
- An improved dust emission model – Part 1: Model description and comparison against measurements (2014, methodology): “In the next three sections, we derive these dependencies through a combination of insights from previous studies, new theoretical work, and simulations with the numerical saltation model COMSALT (Kok and Renno, 2009).”
- The Physics of Sediment Transport Initiation, Cessation, and Entrainment Across Aeolian and Fluvial Environments (2020, methodology): “, 2017] and ejection dynamics [McElwaine et al., 2004; Crassous et al., 2007; Kok and Renno, 2009; Valance and Crassous, 2009; Ho et al., 2012; Comola and Lehning, 2017; Lämmel et al., 2017].”
- An improved parameterization of wind‐blown sand flux on Mars that includes the effect of hysteresis (2010, methodology): “The trajectory of the particle is determined mainly by gravity and fluid drag, and I thus neglect secondary forces due to particle spin, electrostatics, turbulence, and interparticle collisions [Kok and Renno, 2008, 2009b].”