Comparative Analysis of Four Second-Moment Turbulence Closure Models for the Oceanic Mixed Layer

By H. Burchard, Karsten Bolding. 2001

272 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change, Oceanography

View Paper: https://www.semanticscholar.org/paper/a27194889e0165cb0b80aaadbfa861859934c714

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Atmospheric Science

1. L. Umlauf
2. H. Burchard
3. J. Sharples
4. Oliver N. Ross
5. Johannes Gemmrich
6. W. Smyth
7. Dale B. Haidvogel
8. H. van Haren

In Global and Planetary Change

1. L. Umlauf
2. J. Sharples
3. Oliver N. Ross
4. H. Burchard
5. Dale B. Haidvogel

In Oceanography

1. L. Umlauf
2. Oliver N. Ross
3. H. Burchard
4. J. Sharples
5. Johannes Gemmrich
6. W. Smyth
7. Dale B. Haidvogel
8. A. Sogachev

Citations in the corpus

• Vertical mixing schemes in the coastal ocean: Comparison of the level 2.5 Mellor‐Yamada scheme with an enhanced version of the K profile parameterization (2004, background): “[3] Numerous comparisons between vertical mixing parameterizations have been undertaken [Price et al., 1986; Large et al., 1994; Kantha and Clayson, 1994; Large and Gent, 1999; Burchard and Bolding, 2001; Wijesekera et al., 2003].”
• Phytoplankton motility and the competition for nutrients in the thermocline (2007, methodology): “The present study used a 2-equation model of the k-ε variety (Canuto et al. 2001, Sharples et al. 2006), which has been shown to be equivalent (Burchard & Bolding 2001) to the 2-equation MellorYamada (MY) model used by Simpson et al. (1996) (Mellor & Yamada 1982).”
• Second-order turbulence closure models for geophysical boundary layers. A review of recent work (2005, background): “It should be noted that, in order to allow for a source term for dissipation rate equation (39), in the case of free convection with P ¼ 0 and G40; a positive value ce3; of similar magnitude as ce1; has been proposed for the e-equation (39) (see e.g. Rodi, 1980; Burchard and Bolding, 2001).”
• Simulating the Wave-Enhanced Layer under Breaking Surface Waves with Two-Equation Turbulence Models (2001, background): “All equations are discussed in detail in Burchard and Bolding (2001) and are thus not given here.”
• A generic length-scale equation for geophysical turbulence models (2003, methodology): “As an example, we discuss a stability function recently suggested by Canuto et al. (2001), which simpli(cid:142) es in the absence of strati(cid:142) cation according to (see Burchard and Bolding, 2001).”
• Observational and numerical modeling methods for quantifying coastal ocean turbulence and mixing (2008, background): “For a comparative study of various sets of stability functions, see Burchard and Bolding (2001) and Umlauf and Burchard (2005).”