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Investigating the Dependence of Radiative Feedbacks on Patterns of Forcing and Surface Temperature Change
Radiative feedbacks robustly vary over time in transient warming simulations. Published studies offer two explanations: (i) evolving patterns of ocean heat uptake (OHU) or radiative forcing give rise to OHU or forcing efficacies, and (ii) evolving patterns of surface temperature change. This study seeks to determine whether ...