A Technical Guide to MOM4

By S. Griffies, M. Harrison, R. Pacanowski, A. Rosati, Zhi-Pei Liang, M. Schmidt, H. Simmons, R. Slater. 2004

464 citations recorded by the source corpus.

View Paper: https://www.semanticscholar.org/paper/2dc3cbca1c480d1f339e4476d09d35a5cbaa0fd7

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

1. I. Held
2. Ming Zhao
3. Alistair Adcroft
4. L. Harris
5. J. Golaz
6. T. Delworth
7. S. Griffies
8. Robert Hallberg

Citations in the corpus

• GFDL's CM2 Global Coupled Climate Models. Part I: Formulation and Simulation Characteristics (2006, methodology): “The ocean model formulation and physical parameterizations are described in detail in Part II and Griffies et al. (2005) and are based on the Modular Ocean Model code (MOM4; Griffies et al.”
• Fundamentals of Ocean Climate Models (2004, methodology): “ALGORITHMS FOR HYDROSTATIC OCEAN MODELS 238 12.1 Summary of the continuous model equations 238 12.2 Budget of linear momentum for a grid cell 239 12.3 Strategies for time stepping momentum 245 12.4 A leap-frog algorithm 249 12.5 Discretization of time tendencies 252 12.6 A time staggered algorithm 2”
• The Role of Bottom Vortex Stretching on the Path of the North Atlantic Western Boundary Current and on the Northern Recirculation Gyre (2007, methodology): “We coupled a two-dimensional global atmospheric EBM with hydrological cycle to a global OGCM (GFDL MOM4; Griffies et al. 2004) and a slab sea ice model (Winton 2000).”
• Indian Ocean Dipole Response to Global Warming: Analysis of Ocean–Atmospheric Feedbacks in a Coupled Model* (2009, methodology): “The oceanic component of the model is based on the Modular Ocean Model version 4 (MOM4) code (Griffies et al. 2003), which has a horizontal resolution of 18 3 18 and 50 vertical layers.”
• Towards a dynamically balanced eddy-resolving ocean reanalysis: BRAN3 (2013, methodology): “The101 key differences between the model used for BRAN2 and BRAN3 are listed102 in Table 1.103 OFAM1 and OFAM2 are configurations of the GFDL Modular Ocean104 Model (Griffies et al., 2004, OFAM1 uses MOM40d; OFAM2 uses MOM4p1).105 To date, all versions of OFAM have been developed for analysis and pr”
• The dynamical core, physical parameterizations, and basic simulation characteristics of the atmospheric component AM3 of the GFDL global coupled model CM3 (2011, background): “with Newton–Raphson iteration, as in Horowitz et al. (2003). Merging the two models consisted mainly of augmenting the tropospheric model with species (in-”
• Structure and Performance of GFDL's CM4.0 Climate Model (2019, methodology): “The ocean component is based on MOM4 (Griffies et al., 2004), using a z-like vertical coordinate and including a mesoscale eddy closure of the Gent-McWilliams form (Gent et al., 1995), except in CM2.”
• A Theory of Deep Stratification and Overturning Circulation in the Ocean (2011, unknown): “0c (Griffies et al. 2004).”