Not exact matches
The estimated increase of observed
global ocean heat content (over the depth range from 0 to 3000 meters)
between the 1950s and 1990s is at least one order of magnitude larger than the increase in
heat content of any other component.
The connection
between global warming and the changes in
ocean heat content has long been a subject of discussion in climate science.
Essentially, Huber and Knutti take the estimated
global heat content increase since 1850, calculate how much of the increase is due to various estimated radiative forcings, and partition the increase
between increasing
ocean heat content and outgoing longwave radiation.