We assess evidence relevant to Earth's equilibrium climate sensitivity per doubling of
atmospheric CO2, characterized by an effective sensitivity S. This evidence includes …

Interglacials, including the present (Holocene) period, are warm, low land ice extent (high
sea level), end‐members of glacial cycles. Based on a sea level definition, we identify …

The modeling of paleoclimate, using physically based tools, is increasingly seen as a strong
out-of-sample test of the models that are used for the projection of future climate changes …

Although detailed age models exist for some marine sediment records of the last glacial
cycle (0–150 ka), age models for many cores rely on the stratigraphic correlation of benthic …

Two interglacial epochs are included in the suite of Paleoclimate Modeling Intercomparison
Project (PMIP4) simulations in the Coupled Model Intercomparison Project (CMIP6). The …

Abstract The Antarctic Ice Sheet (AIS) is out of equilibrium with the current anthropogenic‐
enhanced climate forcing. Paleoenvironmental records and ice sheet models reveal that the …

The Mediterranean basin is sensitive to global sea-level changes and African monsoon
variability on orbital timescales. Both of these processes are thought to be important to the …

Sea-level histories during the two most recent deglacial–interglacial intervals show
substantial differences,–despite both periods undergoing similar changes in global mean …

During glacial terminations, massive iceberg discharges and meltwater pulses in the North
Atlantic triggered a shutdown of the Atlantic Meridional Overturning Circulation (AMOC) …

Abstract Changes in heat transport associated with fluctuations in the strength of the Atlantic
meridional overturning circulation (AMOC) are widely considered to affect the position of the …