Inverse Analysis Adjustment of the SOC Air-Sea Flux Climatology Using Ocean Heat Transport Constraints

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Global Ocean Meridional Overturning (2007, background): “The ocean appears to gain heat over a large zone near 45°–50°S, although errors are large and the net flux is not well determined [WGASF (2001); all products used in this study contain heat gain here except the adjusted National Oceanography Centre product described by Grist and Josey (2003)].”
Earth's Global Energy Budget (2009, methodology): “Several atlases exist of surface f lux data, but they are fraught with global biases of several tens of watts per meter squared in unconstrained VOS observation-based products (Grist and Josey 2003) that show up, especially when net surface flux fields are globally averaged.”
The total meridional heat flux and its oceanic and atmospheric partition (2005, methodology): “As a comparison to these estimates, in Fig. 3 the zonally integrated annual mean values from bulk formulas of Grist and Josey (2003) summed from 90°N are shown.”
A NEW AIR―SEA INTERACTION GRIDDED DATASET FROM ICOADS WITH UNCERTAINTY ESTIMATES (2009, background): “An imbalance of this magnitude is unphysical: Grist and Josey (2003) estimated that every W m−2 of heat input would warm the upper 1000 m of the ocean by around 0.1°C per decade.”