Linear trends (1955 — 2003) of change in ocean heat content per unit surface area (W m — 2) for the 0 to 700 m layer, based on the work of Levitus et al. (2005a). (ipcc.ch)
We can use changes in ocean heat content, for instance, to directly diagnose the global average radiative imbalance in Watts per meter squared by analyzing for different time slices. (judithcurry.com)
This helps us better understand the processes that control changes in ocean heat content.» (constantinealexander.net)