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.
Not exact matches
Gleckler, P.J., K.R. Sperber, and K. AchutaRao, 2006a: The annual cycle of
global ocean heat content:
observed and simulated.
Observed changes in
ocean heat content have now been shown to be inconsistent with simulated natural climate variability, but consistent with a combination of natural and anthropogenic influences both on a
global scale, and in individual
ocean basins.
• It is very likely that anthropogenic forcings have made a substantial contribution to increases in
global upper
ocean heat content (0 — 700 m)
observed since the 1970s (see Figure SPM.6).
The bottom line is that all available
ocean heat content data show that the
oceans and
global climate continue to build up
heat at a rapid pace, consistent with the
global energy imbalance
observed by satellites.
We must maintain and extend the existing
global climate
observing systems [Riser et al., 2016; von Schuckmann et al., 2016] as well as develop improved coupled (
ocean - atmosphere) climate assessment and prediction tools to ensure reliable and continuous monitoring for Earth's energy imbalance,
ocean heat content, and sea level rise.
In a paper, «
Heat Capacity, Time Constant, and Sensitivity of Earth's Climate System» soon to be published in the Journal of Geophysical Research (and discussed briefly at RealClimate a few weeks back), Stephen Schwartz of Brookhaven National Laboratory estimates climate sensitivity using observed 20th - century data on ocean heat content and global surface temperat
Heat Capacity, Time Constant, and Sensitivity of Earth's Climate System» soon to be published in the Journal of Geophysical Research (and discussed briefly at RealClimate a few weeks back), Stephen Schwartz of Brookhaven National Laboratory estimates climate sensitivity using
observed 20th - century data on
ocean heat content and global surface temperat
heat content and
global surface temperature.