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 ne30ne120 before 8/10/16ne120 after 8/10/16Explanation
dtime30 min15 min15 minTimestep used for most physics processes and for coupling between physics and dynamics
se_nsplit2 4 6*dtime/se_nsplit = time between vertical remaps of the semi-Lagrangian vertical coordinate.
se_qsplit1 1 1dtime/(se_nsplit*se_qsplit) = timestep used for tracer advection
se_rsplit4 3 2*dtime/(se_nsplit*se_qsplit*se_rsplit) = timestep used for dynamics calculations
hypervis_subcycle3 4 4dtime/(se_nsplit_se_qsplit*se_rsplit*hypervis_subcycle) = timestep used for hyperviscosity calculation
hypervis_subcycle_q111dtime/(se_nsplit_se_qsplit*se_rsplit*hypervis_subcycle_q) = timestep used for hyperviscosity calculation in tracer advection (namelist_definition.xml indicates that only '1' is supported in CAM?)
cld_macmic_num_steps6 3* 3Number of times the code surrounding macrophysics + microphysics is subcycled. This means that dtime/cld_macmic_num_steps = timestep used for macrophysics and microphysics.
clubb_timestep300 sec 300 sec 300 secI'm not sure what this means or how it relates to cld_macmic_num_steps
IRADSW2 steps  4 steps (1 hr)4 steps (1 hr)How frequently to compute SW radiation (in multiples of dtime). Radiation tendencies are taken from previous steps for steps when radiation is not recalculated. I think some scaling is made to account for zenith angle changes?
IRADLW2 steps 4 steps 4 stepsHow frequently to compute LW radiation (in multiples of dtime). Radiation tendencies are taken from previous steps for steps when radiation is not recalculated. 
  *since AV1C-04*suggest to use