A global overview of glacier advances and retreats (grouped by regions and by millennia)
for the Holocene is compiled from previous studies. The reconstructions of glacier …

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 …

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

Antarctic volume changes during the past 21 thousand years are smaller than previously
thought, and here we construct an ice sheet history that drives a forward model prediction of …

Global sea level provides an important indicator of the state of the warming climate, but
changes in regional sea level are most relevant for coastal communities around the world …

Holocene relative sea-level (RSL) records exhibit spatial and temporal variability that arises
mainly from the interaction of eustatic (land ice volume and thermal expansion) and isostatic …

Since 1995 several ice shelves in the Northern Antarctic Peninsula have collapsed and
triggered ice-mass unloading, invoking a solid Earth response that has been recorded at …

This paper compiles and reviews marine and terrestrial data constraining the dimensions
and configuration of the Antarctic Peninsula Ice Sheet (APIS) from the Last Glacial Maximum …

The existence of a thin, weak asthenospheric layer beneath Earth's lithospheric plates is
consistent with existing geological and geophysical constraints, including Pleistocene glacio …

Recognition of how dynamic the Antarctic ice sheets and glaciers were during the late
Holocene has grown in recent years. Proxy data suggests the presence of Neoglacial …