Ocean ventilation is the transfer of tracers and young water from the surface down into the
ocean interior. The tracers that can be transported to depth include anthropogenic heat and …

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 effective climate sensitivity (EffCS) of models in the Coupled Model Intercomparison
Project 6 (CMIP6) has increased relative to CMIP5. We explore the implications of this for …

Cross-equatorial ocean heat transport (OHT) changes have been found to damp meridional
shifts of the intertropical convergence zone (ITCZ) induced by hemispheric asymmetries in …

The ocean absorbs most of the excess heat from anthropogenic climate change, causing
global ocean warming and sea-level rise with a series of consequences for human society …

Atmosphere‐ocean general circulation models (AOGCMs) struggle to reproduce recently
observed sea surface temperature (SST) trend patterns. Here, we quantify the relevance of …

Abstract The Ocean Heat Uptake Efficiency (OHUE) quantifies the ocean's ability to mitigate
surface warming through deep heat sequestration. Despite its importance, the main controls …

Barystatic sea level rise (SLR) caused by the addition of freshwater to the ocean from
melting ice can in principle be recorded by a reduction in seawater salinity, but detection of …

Proxy reconstructions suggest that increasing global mean sea surface temperature
(GMSST) during the last deglaciation was accompanied by a comparable or greater …

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 …