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The possibility of using global mean near-surface temperature, its rate of change or the global mean ocean heat-flux as predictors to statistically estimate the change of global mean sea-level is explored in the context of a long climate simulation of the past millennium with the climate model ECHO-G. Such relationships have recently been proposed to by-pass the difficulty of estimating future sea-level...
The climate system is excited by changes in the solar forcing caused by two effects: (a) by variations of the solar radiation caused by dynamical processes within the Sun, and (b) by changes in the orbital parameters of the Earth around the Sun.Numerical simulations with a three-dimensional coupled ocean–atmosphere climate model have been performed to investigate the sensitivity of the climate system...
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