The Eurasian ice sheet complex (EISC) was the third largest ice mass during the Last
Glacial Maximum with a span of over 4500 km and responsible for around 20 m of eustatic …

Relative sea-level change along the Italian coast and adjacent seas—the combined result of
eustasy, glacio-hydro-isostasy and vertical tectonic motion—exhibits considerable spatial …

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

Global mean sea level is an integral of changes occurring in the climate system in response
to unforced climate variability as well as natural and anthropogenic forcing factors. Its …

With polar temperatures∼ 3–5° C warmer than today, the last interglacial stage (∼ 125 kyr
ago) serves as a partial analogue for 1–2° C global warming scenarios. Geological records …

Theory has suggested that the West Antarctic Ice Sheet may be inherently unstable. Recent
observations lend weight to this hypothesis. We reassess the potential contribution to …

Sea-level change in the Mediterranean Sea during glacial cycles is determined by the
temporally variable eustatic change and by the spatially variable glacio-hydro-isostatic …

Sea-level variations spread over a very broad spectrum of spatial and temporal scales as a
result of complex processes occurring in the Earth System in response to natural variability …

Global mean sea level has been steadily rising over the last century, is projected to increase
by the end of this century, and will continue to rise beyond the year 2100 unless the current …

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 …