Available output for cube22 to cube42 cs510 integrations # 6-hourly 2-D fields: # ==================== # # ETAN Perturbation of Surface (pressure, height) (Pa,m) # PHIBOT ocean bottom pressure / top. atmos geo-Potential # TAUX zonal surface wind stress, >0 increases uVel # TAUY meridional surf. wind stress, >0 increases vVel # TFLUX net surface heat flux, >0 increases theta # SFLUX net surface salt flux, >0 increases salt # prior to cube43, SFLUX is equal to SRELAX plus salt # rejected by sea ice # KPPhbl KPP boundary layer depth, bulk Ri criterion # KPPmld Mixed layer depth, dT=.8degC density criterion # SSS Sea Surface Salinity (g/kg) # SST Sea Surface Temperature (degC,K) # UVEL_k2 Zonal Component of Velocity at level 2 (m/s) # VVEL_k2 Meridional Component of Velocity at level 2 (m/s) # # daily 2-D fields: # =================== # # AREAtave.*.data : fractional sea ice area # HEFFtave.*.data : effective sea ice thickness in m # UICEtave.*.data : zonal sea ice velocity in m/s # VICEtave.*.data : meridional sea ice velocity in m/s # EmPmRtave.*.data : following are surface flux diagnostics, # QNETtave.*.data : some redundant, some not, see below # QSWtave.*.data : # FUtave.*.data : # FVtave.*.data : # C pkg/diagnostics SIempmr, dumpfreq EmPmR, and tavefreq EmPmRtave C are identical but they differ from pkg/diagnostics EXFempmr, which C is EmPmR before impact of ice. # C SIqnet, Qnet, and QNETtave are identical. C With #undef NONLIN_FRSURF SIqnet is identical to -(TFLUX-TRELAX). C Except over land and under sea ice, SIqnet is also identical to C EXFlwnet+EXFswnet-EXFhl-EXFhs. # C SIqsw, Qsw, and QSWtave are identical. C Except under sea ice, SIqsw is also identical to EXFswnet. # C pkg/diagnostics SIfu and TAUX, dumpfreq FU, and tavefreq FUtave C are identical but they differ from pkg/diagnostics EXFtaux, which C is stress before impact of ice. Also when using exf bulk C formulae, EXFtaux is defined on tracer rather than uvel points. # C pkg/diagnostics SIfv and TAUY, dumpfreq FV, and tavefreq FVtave C are identical but they differ from pkg/diagnostics EXFtauy, which C is stress before impact of ice. Also when using exf bulk C formulae, EXFtauy is defined on tracer rather than vvel points. # # monthly 2-D fields: # =================== # # ETANSQ Square of Perturbation of Sfc (Pa2,m2) # SRELAX surface salinity relaxation, >0 increases salt # EXFhs Sensible heat flux into ocean # EXFhl Latent heat flux into ocean # EXFlwnet Net longwave radiation # EXFswnet Net shortwave radiation # # monthly 3-D fields: # =================== # # SALTanom Salt anomaly (=SALT-35; g/kg) # THETA Potential Temperature (degC,K) # UVEL Zonal Component of Velocity (m/s) # VVEL Meridional Component of Velocity (m/s) # UVELMASS Zonal Mass-Weighted Comp of Velocity (m/s) # VVELMASS Meridional Mass-Weighted Comp of Velocity (m/s) # WVELMASS Vertical Mass-Weighted Comp of Velocity (m/s) # # SALTSQan Square of Salt anomaly (=(SALT-35)^2 (g^2/kg^2) # THETASQ Square of Potential Temperature (K2) # UVELSQ Square of Zonal Comp of Velocity (m2/s2) # VVELSQ Square of Meridional Comp of Velocity (m2/s2) # WVELSQ Square of Vertical Comp of Velocity (m2/s2) # UV_VEL_Z Meridional Transport of Zonal Momentum (m2/s2) # WU_VEL Vertical Transport of Zonal Momentum (m^2/s^2) # WV_VEL Vertical Transport of Meridional Momentum (m^2/s^2) # # UTHMASS Zonal Mass-Weight Transp of Pot Temp (K.m/s) # VTHMASS Meridional Mass-Weight Transp of Pot Temp (K.m/s) # WTHMASS Vertical Mass-Weight Transp of Pot Temp (K.m/s) # USLTMASS Zonal Mass-Weight Transp of Salt (g/kg.m/s) # VSLTMASS Meridional Mass-Weight Transp of Salt (g/kg.m/s) # WSLTMASS Vertical Mass-Weight Transp of Salt (g/kg.m/s) # # RHOAnoma Density Anomaly (=Rho-rhoConst; kg/m^3) # DRHODR Stratification: d.Sigma/dr (kg/m3/r_unit; kg/m^4) # RHOANOSQ Square of Density Anomaly (=(Rho-rhoConst)^2; kg^2/m^6) # URHOMASS Zonal Transport of Density (kg/m^2/s) # VRHOMASS Meridional Transport of Density (kg/m^2/s) # WRHOMASS Vertical Transport of Potential Density (kg/m^2/s) # # VISCA4 Biharmonic Viscosity Coefficient in (m4/s)