To quantify climate change, researchers need to know the Transient Climate Response (TCR) and Equilibrium Climate Sensitivity (ECS) of Earth.
Both values are projected global mean surface temperature changes in response to doubled atmospheric carbon dioxide concentrations but on different timescales.
There have been many attempts to determine TCR and ECS values based on the history of temperature changes over the last 150 years and the measurements of important climate drivers, such as carbon dioxide, researchers said.
It is well known that aerosols such as those emitted in volcanic eruptions act to cool Earth, at least temporarily, by reflecting solar radiation away from the planet.
In a similar way, land use changes such as deforestation in northern latitudes result in bare land that increases reflected sunlight.
However, assumptions made to account for these drivers are too simplistic and result in incorrect estimates of TCR and ECS, said study co-author Gavin Schmidt, the director of NASA's Goddard Institute for Space Studies (GISS) in New York.
In a NASA first, researchers at GISS accomplished such a feat as they calculated the temperature impact of each of these variables - greenhouse gases, natural and manmade aerosols, ozone concentrations, and land use changes - based on historical observations from 1850 to 2005 using a massive ensemble of computer simulations.
Since earlier studies do not account for what amounts to a net cooling effect for parts of the northern hemisphere, TCR and ECS predictions have been lower than they should be.
This means that Earth's climate sensitivity to carbon dioxide - or atmospheric carbon dioxide's capacity to affect temperature change - has been underestimated, researchers said.
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