In the present model, the OHC estimates are calculated from 5 km resolution sea surface temperatures (SST) obtained from NESDIS GEO-POLAR Blended SST Analyses (Harris and Maturi, 2012) combined with Jason-2, SARAL and Cyrosat-2 altimeter estimates of the 20°C and 26°C isotherm depths; the altimeter estimates are derived from a scheme using a daily ocean climatology of mean isotherm depths and reduced gravities. Based on a mean ratio between the 20°C and 26°C isotherm depths, the depth of the 26°C isotherm and the ocean mixed layer depth are inferred. By integrating the 26°C isotherm depth to the surface (where SST is the surface boundary condition) an OHC is calculated. The product fields are evaluated monthly when thermal structure data from various ocean data collection platforms become available (e.g. Argo floats, XBT transects, mooring measurements, and airborne profiling from NOAA research aircraft).
Satellite derived OHC is currently produced operationally for the North Atlantic, North Pacific, and South Pacific. A suite of Ocean Heat Content Products are planned for the North and South Indian Oceans.
As new altimeters are available, they will be incorporated into the Oceanic Heat Content algorithm for product generation.