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 …

Sea surface temperatures (SSTs) recorded by alkenones and oxygen isotopes in the
Alboran basin are used here to describe, at an unprecedented fine temporal resolution, the …

Improved knowledge of glacial-to-interglacial global temperature change yields Charney
(fast-feedback) equilibrium climate sensitivity 1.2±0.3° C (2σ) per W/m2, which is 4.8° C±1.2° …

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 …

Considerable ambiguity remains over the extent and nature of millennial/centennial-scale
climate instability during the Last Interglacial (LIG). Here we analyse marine and terrestrial …

Contourites in the Gulf of Cádiz (GC) preserve a unique archive of Mediterranean Outflow
Water (MOW) variability over the past 5.3 Ma. In our study, we investigate the potential of …

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 …

Deep ocean circulation has been considered relatively stable during interglacial periods, yet
little is known about its behavior on submillennial time scales. Using a subcentennially …

The rate and consequences of future high latitude ice sheet retreat remain a major concern
given ongoing anthropogenic warming. Here, new precisely dated stalagmite data from NW …

There is limited understanding of temperature and atmospheric circulation changes that
accompany an Atlantic Meridional Overturning Circulation (AMOC) slowdown beyond the …