Evaluation of the Simulated Interannual and Subseasonal Variability in an AMIP-Style Simulation Using the CSU Multiscale Modeling Framework

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The Role of Convective Moistening in the Madden–Julian Oscillation (2009, background): “In contrast, the SP-CAM produces extremely vigorous MJOs, stronger even than most of the observed disturbances (Khairoutdinov et al. 2008; Benedict and Randall 2009).”
Surface Fluxes and Tropical Intraseasonal Variability: a Reassessment (2008, methodology): “The off-equatorial ”red spots” in the stronger-MJO models are qualitatively consistent with similar structures found in simulations under the multiscale modeling framework (”SP-CAM”; Khairoutdinov et al. 2008), which also has a strong MJO compared to that in most GCMs.”
CORRIGENDUM of the MJO Transition from Shallow to Deep Convection in Cloudsat-Calipso Data and GISS GCM Simulations (2012, background): “…convection and humidity because of strong convective entrainment or rain evaporation (Bechtold et al. 2008; Kim et al. 2009, 2011a; Hannah and Maloney 2011) or that embed a cloud-resolving model within GCM gridboxes (Khairoutdinov et al. 2008; Thayer-Calder and Randall 2009; Zhu et al. 2009).”
Structure of the Madden-Julian Oscillation in the Superparameterized CAM (2009, methodology): “Although great progress has been made in using a global CRM to produce a single but realistic MJO (e.g., Miura et al. 2007), simulations of sufficient duration to analyze systematic MJO behavior— ideally, multiple years—remain computationally prohibitive (Khairoutdinov et al. 2008, hereafter KDR08).”