Tropical Pacific and Atlantic Climate Variability in CCSM3

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On the origin of equatorial Atlantic biases in coupled general circulation models (2008, background): “May (MAM), which leads to a spurious double-ITCZ in the annual mean (Breugem et al. 2006; Deser et al. 2006; Stockdale et al. 2006).”
Last Glacial Maximum and Holocene Climate in CCSM3 (2006, unknown): “4 region (5°S–5°N, 170°– 120°W) is presented as a measure of ENSO activity, as in the present-day CCSM3 simulations (Deser et al. 2006).”
Multimodel Ensemble ENSO Prediction with CCSM and CFS (2009, result): “Although it is difficult to detect in this figure, the ENSO events in CCSM tend to extend too far into the western Pacific compared to the observational data (please see Deser et al. 2006, their Figs.”
The Impact of Convection on ENSO: From a Delayed Oscillator to a Series of Events (2008, background): “There are two things worth noting: the easterly anomalies are too strong, compared to observations (see Deser et al. 2006, their Fig.”
The Low-Resolution CCSM3 (2006, background): “ENSO is not particularly well simulated in T85x1 (Deser et al. 2005), so the hope for T31x3 in this regard is only that its associated interannual SST variance not be significantly worse than at either of the two higher resolutions.”