On the representation of high latitude processes in the ORCA-LIM global coupled sea ice–ocean model

By R. Timmermann, Hugues Goosse, Gurvan Madec, T. Fichefet, C. Ethe, V. Dulière. 2005

283 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change, Oceanography

View Paper: https://www.semanticscholar.org/paper/ead39327ccca715baf066c51e15c812d09e30ba9

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. Sandrine Bony
2. J. Dufresne
3. Martin Losch
4. V. Dulière
5. I. Musat
6. Hugues Goosse
7. Eric Guilyardi
8. A. Idelkadi

In Global and Planetary Change

1. Sandrine Bony
2. J. Dufresne
3. Martin Losch
4. V. Dulière
5. Corinne Le Quéré
6. E. Buitenhuis
7. T. Hashioka
8. I. Musat

In Oceanography

1. Martin Losch
2. V. Dulière
3. Corinne Le Quéré
4. E. Buitenhuis
5. T. Hashioka
6. L. Brodeau
7. A. Treguier
8. Sandrine Bony

Citations in the corpus

• Modeling ice shelf cavities in a z coordinate ocean general circulation model (2008, methodology): “[38] The Weddell Gyre with a mean transport of a little over 26 Sv is weaker than in other simulations with a s coordinate model [Beckmann et al., 1999; Timmermann et al., 2002a], but stronger than, for example, in the z coordinate model of Timmermann et al. [2005] .”
• An ERA40-based atmospheric forcing for global ocean circulation models (2010, methodology): “The global monthly climatology of continental runoff is the same as used by Timmermann et al. (2005).”
• On the assimilation of ice velocity and concentration data into large-scale sea ice models (2007, methodology): “This method to approach data assimilation into sea ice models is an interesting first step towards real data assimilation into NEMOLIM (Timmermann et al., 2005), a global sea ice-ocean model.”
• The Louvain-La-Neuve sea ice model LIM3.6: global and regional capabilities (2015, background): “LIM2 was later on integrated into the NEMO system, for the global reference configuration ORCA2-LIM (Timmermann et al., 2005).”
• An elastic-viscous-plastic sea ice model formulated on Arakawa B and C grids (2009, methodology): “The version of LIM used in this study (LIM2) is described in full detail in Timmermann et al. (2005) and references therein.”
• Biogeochemical fluxes through mesozooplankton (2006, unknown): “Since the model cannot calculate a meeting of the meridians on the north pole, the grid has been distorted in the northern hemisphere to have two “north poles” over northern Eurasia and North America ( Timmermann et al. , 2005).”
• Key features of the IPSL ocean atmosphere model and its sensitivity to atmospheric resolution (2010, methodology): “The ocean–sea ice interaction is exactly the same when the ocean–ice model is forced by climatology (e.g. see Timmermann et al. 2004) or coupled to an atmosphere model.”
• Combined constraints on global ocean primary production using observations and models (2013, methodology): “It is coupled to a dynamic-thermodynamic sea ice model [Timmermann et al., 2005].”