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) represents an invaluable case study to investigate the
response of components of the Earth system to global warming. However, the scarcity of …

We use numerical climate simulations, paleoclimate data, and modern observations to study
the effect of growing ice melt from Antarctica and Greenland. Meltwater tends to stabilize the …

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 …

Climate models show strong links between Antarctic and global temperature both in future
and in glacial climate simulations. Past Antarctic temperatures can be estimated from …

New high-resolution deuterium excess (d) data from the two EPICA ice cores drilled in
Dronning Maud Land (EDML) and Dome C (EDC) are presented here. The main moisture …

The dominant feature of large-scale mass transfer in the modern ocean is the Atlantic
meridional overturning circulation (AMOC). The geometry and vigour of this circulation …

Abstract The Southern Ocean plays a prominent role in the Earth's climate and carbon cycle.
Changes in the Southern Ocean circulation may have regulated the release of CO2 to the …

Much of our understanding of Cenozoic climate is based on the record of δ18O measured in
benthic foraminifera. However, this measurement reflects a combined signal of global …