Table 2 Perturbed parameters in sensitivity studies in ECHAM6.3-HAM2.3
Sentivitiy runs | Perturbed parameter |
|---|---|
REF | Default diagnostic scheme |
REF-S1 | Reducing autoconversion rate (ccraut) in stratiform clouds from 5 (default value) to 1 → Delayed rain formation in stratiform clouds |
REF-S2 | Reducing threshold RH \({{{{{\boldsymbol{\eta }}}}}}_{{{{{\boldsymbol{crit}}}}}}\) by applying a scaling factor of 0.8, only over the ocean → more marine clouds |
REF-S3 | Increasing evaporation of raindrops to 200% of default evaporation rate → Increase RH and therefore cloud cover |
REF-S4 | Reducing entrainment rate for shallow convective clouds (entrscv) from 0.003 to 0.001 → Drying the boundary layer and reducing cloud cover |
REF-S5 | Reducing fraction of overshooting of shallow convection (cmfctop) from 0.2 to 0.1 → Keeping more moisture in the planetary boundary layer |
REF-S6 | Reducing autoconversion rate for convective clouds (cprcon) from 0.0009 to 0.00002 → Delayed rain formation in convective clouds |
PROG_CC | Default prognostic scheme |
PROG_CC-S1 | Reducing scaling factor for cloud formation by mixing of detrained air with environmental cloud-free air (tuningDetrainedMixing) from 0.8 (default value) to 0.6 → Reducing cloud formation |
PROG_CC-S2 | Reducing scaling factor for entrainment rate for shallow convection (tuningConvEntrShallow) from 0.003 (default value) to 0.0003 → Drying the boundary layer and reducing cloud cover |
PROG_CC-S3 | Increasing scaling factor for turbulent mixing (tuningTurbulentMixing) from 0.0 (default value) to 1.0 → Affect cloud formation |
PROG_CC-S4 | Reducing critical RH at the surface above which large-scale cloud cover can form (tuningRHcritSurface) from 0.9 (default value) to 0.8 everywhere → more clouds |