A global compilation of glacier advances and retreats for the past two millennia grouped by
17 regions (excluding Antarctica) highlights the nature of glacier fluctuations during the late …

Geophysical ice-sheet models are used to predict future ice-sheet dimensions and, in turn,
these projections help estimate the magnitude of eustatic sea-level rise. Before models can …

The sensitivity of the Greenland ice sheet to climate forcing is of key importance in assessing
its contribution to past and future sea level rise. Surface mass loss occurs during summer …

The sensitivity of the Northeast Greenland Ice Stream (NEGIS) to prolonged warm periods is
largely unknown and geological records documenting such long-term changes are needed …

To determine the long-term sensitivity of the Greenland ice sheet to a warmer climate, we
explored how it responded to the Holocene thermal maximum (8–5 cal. kyr BP; calibrated to …

The melting of marine terminating glaciers in Northeast Greenland is a visible sign that our
climate is changing. This melt has been partly attributed to changes in oceanic heat fluxes …

Abstract During the Last Interglacial (LIG) period, between 130 and 116 thousand years
before present (ka BP), the Greenland Ice Sheet (GrIS) was considerably reduced in size …

The Greenland Ice Sheet is a large contributor to global sea-level rise, and current mass
losses are projected to accelerate. However, model projections of future ice-sheet evolution …

We present a reconstruction of the timing and retreat rates of more than 2000 m thick
Younger Dryas (YD) fjord glaciers in western Norway using a detailed chronology of 10Be …

The possible demise of the Greenland ice sheet and its effect on global sea level rank
among the most serious climate threats to society. To improve our knowledge about the …