We present a new reconstruction of the Antarctic Ice Sheets between 20 ka BP and the
present day. Our reconstruction is derived using a numerical model to generate a physically …

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 …

To understand how planet Earth works we study it increasingly as a system–a collection of
interdependent parts or spheres–the lithosphere, the hydrosphere, the cryosphere, the …

We present a glacial isostatic adjustment (GIA) model for Antarctica. This is driven by a new
deglaciation history that has been developed using a numerical ice-sheet model, and is …

The rate and magnitude of the Antarctic Ice Sheet (AIS) contribution to global sea-level rise
beyond 2100 ce remains highly uncertain. Past changes of the AIS, however, offer …

The prediction of crustal motions and gravity change driven by glacial isostatic adjustment
(GIA) in Antarctica is critically dependent on the reconstruction of the configuration and …

The Antarctic Peninsula is one of the three fastest warming regions on Earth. Here we
review Holocene proxy records of marine and terrestrial palaeoclimate in the region, and …

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 …

Precise relative sea level (RSL) data are important for inferring regional ice sheet histories,
as well as hel** to validate numerical models of ice sheet evolution and glacial isostatic …

The rapidly retreating Thwaites and Pine Island glaciers together dominate present-day ice
loss from the West Antarctic Ice Sheet and are implicated in runaway deglaciation scenarios …