2 Chapter 2 assesses observed large-scale changes in climate system drivers, key climate
indicators and 3 principal modes of variability. Chapter 3 considers model performance and …

During the last interglacial (LIG) period, global mean sea level (GMSL) was higher than at
present, likely driven by greater high-latitude insolation. Past sea-level estimates require …

Past sea-level change represents the large-scale state of global climate, reflecting the
waxing and waning of global ice sheets and the corresponding effect on ocean volume …

A substantially updated version of the correlation table showing chronostratigraphical
subdivisions of late Cenozoic geological time, spanning the last 2.7 million years is …

Prior to inferring ice sheet stability from past interglacial sea-level records, these records
must first be corrected for the contaminating effects of glacial isostatic adjustment (GIA) …

Abstract The last interglacial (LIG;~ 130 to~ 118 thousand years ago, ka) was the last time
global sea level rose well above the present level. Greenland Ice Sheet (GrIS) contributions …

Polar temperatures during the Last Interglacial [LIG;~ 129 to 116 thousand years (ka)] were
warmer than today, making this time period an important testing ground to better understand …

It is generally agreed that the Last Interglacial (LIG;∼ 130–115 ka) was a time when global
average temperatures and global mean sea level were higher than they are today. However …

Abstract The Last Interglacial (LIG: 130,000–115,000 years ago) was a period of warmer
global mean temperatures and higher and more variable sea levels than the Holocene …

Previous studies have interpreted Last Interglacial (LIG;∼ 129–116 ka) sea‐level estimates
in multiple different ways to calibrate projections of future Antarctic ice‐sheet (AIS) mass loss …