Spurious dianeutral mixing and the role of momentum closure

By Mehmet Ilıcak, Alistair Adcroft, S. Griffies, Robert Hallberg. 2012

167 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change, Oceanography

View Paper: https://www.semanticscholar.org/paper/60c9f934c70e66132861d52ab20b7646c3f10225

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. Robert Hallberg
2. S. Griffies
3. Gokhan Danabasoglu
4. B. Fox‐Kemper
5. Mathew E. Maltrud
6. S. Yeager
7. C. Böning
8. Alistair Adcroft

In Global and Planetary Change

1. Robert Hallberg
2. S. Griffies
3. Gokhan Danabasoglu
4. B. Fox‐Kemper
5. Alistair Adcroft
6. Sonya Legg
7. S. Yeager
8. Mathew E. Maltrud

In Oceanography

1. Robert Hallberg
2. S. Griffies
3. Gokhan Danabasoglu
4. B. Fox‐Kemper
5. Alistair Adcroft
6. Raffaele Ferrari
7. C. Böning
8. Mathew E. Maltrud

Citations in the corpus

• Sensitivity of the Ocean State to the Vertical Distribution of Internal-Tide-Driven Mixing (2013, background): “The absence of spurious mixing associated with advection in the isopycnal coordinates (Griffies et al. 2000; Ilicak et al. 2012) facilitates study of the effects of changing the diapycnal mixing parameterization.”
• Seamless cross-scale modeling with SCHISM (2016, methodology): “1 and 2 of Ilicak et al. (2012) , we remark that SCHISM results show less noise (using GOLD results as benchmark) especially at higher resolution.”
• A multi-resolution approach to global ocean modeling (2013, methodology): “On the second research track we will develop a robust test-suite following Ilicak et al. (2012) to carefully quantify the fidelity of the underlying numerical approach in ocean-specific configurations.”
• Using a resolution function to regulate parameterizations of oceanic mesoscale eddy effects (2013, background): “However, there are substantial ancillary benefits of using a Gent–McWilliams diffusivity in depth-coordinate B-grid ocean models: it suppresses the well-known checkerboard null mode in the density field, and it suppresses numerical diapycnal mixing arising from advective truncation errors arising fr”
• Challenges and Prospects in Ocean Circulation Models (2019, background): “Isopycnal coordinates suppress numerical diffusion (White et al., 2009; Ilicak et al., 2012), and when combined with suitable physical parameterizations of the mixing in the bottom boundary layer (Legg et al.”