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 …

Abstract The Last Interglacial (LIG, 129–116 thousand of years BP, ka) represents a test bed
for climate model feedbacks in warmer-than-present high latitude regions. However, mainly …

Late Pleistocene sea level has been reconstructed from ocean sediment core data using a
wide variety of proxies and models. However, the accuracy of individual reconstructions is …

The last interglaciation (LIG, 129 to 116 thousand years ago) was the most recent time in
Earth's history when global mean sea level was substantially higher than it is at present …

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 …

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 …

Abstract The Last Interglacial (LIG) represents an invaluable case study to investigate the
response of components of the Earth system to global warming. However, the scarcity of …

Coinciding with global warming, Arctic sea ice has rapidly decreased during the last four
decades and climate scenarios suggest that sea ice may completely disappear during …

A Community Climate System Model, Version 3 (CCSM3) simulation for 125 ka during the
Last Interglacial (LIG) is compared to two recent proxy reconstructions to evaluate surface …