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evaporation, > 0 decreases salinity
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EXF Net shortwave radiation, >0 decreases theta
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GM Bolus transport stream-function : X component
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GM Bolus transport stream-function : Y component
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Hydrostatic (ocean) pressure / (atmos) geo-Potential
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KPP boundary layer depth, bulk Ri criterion
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KPP vertical eddy viscosity coefficient
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K_31 element (W.point, X.dir) of GM-Redi tensor
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K_32 element (W.point, Y.dir) of GM-Redi tensor
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K_33 element (W.point, Z.dir) of GM-Redi tensor
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Latent heat flux into ocean, >0 increases theta
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meridional 10-m wind speed
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Meridional Component of Velocity (m/s)
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Meridional Component of Velocity at level 2 (m/s)
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Meridional Mass-Weighted Comp of Velocity (m/s)
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meridional surf. wind stress, >0 increases vVel
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Mixed layer depth, dT=.8degC density criterion
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Net longwave radiation, >0 decreases theta
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net surface heat flux, >0 increases theta
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net surface salt flux, >0 increases salt
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Nonlocal transport coefficient
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ocean bottom pressure / top. atmos geo-Potential
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Perturbation of Surface (height) (m)
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Potential Density Anomaly (=Rho-rhoConst)
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Potential Temperature (degC)
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Salt mixing ratio (g/kg)
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Sea Surface Salinity (g/kg)
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Sea Surface Temperature (degC)
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Sensible heat flux into ocean, >0 increases theta
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Short-wave flux fraction penetrating mixing layer
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snow precipitation, > 0 decreases salinity
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Squarex1 of Perturbation of Sfc (m^2)
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Stratification: d.Sigma/dr (kg/m3/r_unit)
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surface (2-m) air temperature
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surface (2-m) specific humidity
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surface salinity relaxation, >0 increases salt
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Vertical Component of Velocity (m/s)
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Vertical diffusion coefficient for heat
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Vertical diffusion coefficient for salt & tracers
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Vertical Mass-Weighted Comp of Velocity (m/s)
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zonal 10-m wind speed
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Zonal Component of Velocity (m/s)
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Zonal Component of Velocity at level 2 (m/s)
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Zonal Mass-Weighted Comp of Velocity (m/s)
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zonal surface wind stress, >0 increases uVel
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