Glacial isostatic adjustment (GIA) describes the response of the solid Earth, the gravitational
field, and the oceans to the growth and decay of the global ice sheets. A commonly studied …

Changes in the strength and position of Southern Hemisphere westerly winds during the
Last Glacial cycle have been invoked to explain both millennial and glacial–interglacial …

A comprehensive database of paleoclimate records is needed to place recent warming into
the longer-term context of natural climate variability. We present a global compilation of …

Abstract The European Project for Ice Coring in Antarctica Dome ice core from Dome C
(EDC) has allowed for the reconstruction of atmospheric CO2 concentrations for the last …

We combined an ensemble of satellite altimetry, interferometry, and gravimetry data sets
using common geographical regions, time intervals, and models of surface mass balance …

Water-stable isotopes in polar ice cores are a widely used temperature proxy in
paleoclimate reconstruction, yet calibration remains challenging in East Antarctica. Here, we …

ABSTRACT A new model of the deglaciation history of Antarctica over the past 25 kyr has
been developed, which we refer to herein as ICE-6G_C (VM5a). This revision of its …

A high-resolution deuterium profile is now available along the entire European Project for
Ice Coring in Antarctica Dome C ice core, extending this climate record back to marine …

Paleoclimate data show that climate sensitivity is~ 3 deg-C for doubled CO2, including only
fast feedback processes. Equilibrium sensitivity, including slower surface albedo feedbacks …

The cause of warming in the Southern Hemisphere during the most recent deglaciation
remains a matter of debate,. Hypotheses for a Northern Hemisphere trigger, through oceanic …