We investigate the dependence of radiative feedback on the pattern of sea‐surface
temperature (SST) change in 14 Atmospheric General Circulation Models (AGCMs) forced …

The atmospheric Green's function method is a technique for modeling the response of the
atmosphere to changes in the spatial field of surface temperature. While early studies …

Here, we show that the Last Glacial Maximum (LGM) provides a stronger constraint on
equilibrium climate sensitivity (ECS), the global warming from increasing greenhouse gases …

Predicting forced, long‐term radiative feedbacks from internal climate variability has been a
decades‐long quest in climate science. We train a convolutional neural network (CNN) to …

This study assesses the effective climate sensitivity (EffCS) and transient climate response
(TCR) derived from global energy budget constraints within historical simulations of eight …

Quantifying the net carbon flux from land use and land cover changes (f LULCC) is critical
for understanding the global carbon cycle and, hence, to support climate change mitigation …

Livestock agriculture accounts for∼ 15% of global anthropogenic greenhouse gas (GHG)
emissions. Recently, natural climate solutions (NCS) have been identified to mitigate farm …

Climate models suggest that the climate feedback parameter λ, which denotes the
magnitude of the Earth radiative response to a change in global surface temperature, varies …

The magnitude of global surface temperature change in response to unit radiative forcing
depends on the type and magnitude of forcing agent—a concept known as a “forcing …

The realization that atmospheric radiative feedbacks depend on the underlying patterns of
surface warming and global temperature, and thus, change over time has lead to a …