Diurnal Coupling in the Tropical Oceans of CCSM3

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The Low-Resolution CCSM3 (2006, methodology): “The ocean component (Danabasoglu et al. 2006) has two possible resolutions; nominal 1° horizontal with 40 vertical levels and nominal 3° horizontal with 25 levels, which has roughly 17 times fewer grid points.”
The Impact of Abyssal Mixing Parameterizations in an Ocean General Circulation Model (2009, background): “…(POP 1.4.3) ( Smith et al. 1992) that is the ocean component of the Community Climate System Model, version 3 (CCSM3; see Smith and Gent 2002; Collins et al. 2006; Danabasoglu et al. 2006; Gent et al. 2006, for a description), which is based at the National Center for Atmospheric Research (NCAR).”
Multimodel Ensemble ENSO Prediction with CCSM and CFS (2009, background): “0 (Collins et al. 2006a,b; Kiehl et al. 2006; Large and Danabasoglu 2006; Danabasoglu et al. 2006; Meehl et al. 2006) and the CFS (Saha et al. 2006; Wang et al. 2005), are coupled ocean–atmosphere–land models whose formulations of dynamics and subgrid-scale physical parameterizations, in both the…”
Atmosphere‐ocean coupled processes in the Madden‐Julian oscillation (2015, result): “Since CGCM mean state errors can degrade the simulation of the MJO (section 5.3), we note that several other studies have also found that including the diurnal cycle of air-sea coupling reduced tropical SST and rainfall biases [e.g., Danbasoglu et al., 2006; Ham et al., 2010].”