In panel - b the magnitude of unforced variability is large (wide range between the blue lines) and thus changes in the multidecadal rate of warming could come about due to unforced variabilit
In panel - b the magnitude of unforced variability is large (wide range between the blue lines) and thus
changes in the multidecadal rate of warming could come about due to unforced variabilit
in the
multidecadal rate of warming could come about due to unforced variability.
The near - linear
rate of anthropogenic warming (predominantly from anthropogenic greenhouse gases) is shown
in sources such as: «Deducing
Multidecadal Anthropogenic Global Warming Trends Using Multiple Regression Analysis» «The global warming hiatus — a natural product of interactions of a secular warming trend and a multi-decadal oscillation» «The Origin and Limits of the Near Proportionality between Climate Warming and Cumulative CO2 Emissions» «Sensitivity of climate to cumulative carbon emissions due to compensation of ocean heat and carbon uptake» «Return periods of global climate fluctuations and the pause» «Using data to attribute episodes of warming and cooling
in instrumental records» «The proportionality of global warming to cumulative carbon emissions» «The sensitivity of the proportionality between temperature
change and cumulative CO2 emissions to ocean mixing»