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 new model of the last deglaciation event of the Late Quaternary ice age is here described
and denoted as ICE‐6G_C (VM5a). It differs from previously published models in this …

Using global positioning system, very long baseline interferometry, satellite laser ranging
and Doppler Orbitography and Radiopositioning Integrated by Satellite observations …

The most recently published model of the glacial isostatic adjustment process in the ICE‐NG
(VMX) sequence from the University of Toronto, denoted ICE‐6G_C (VM5a), was originally …

Detectable crustal motion and secular rate of change of solid‐surface gravity may be
produced by the Earth's response to present‐day and past ice mass changes in Antarctica …

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 …

This paper presents the first systematic attempt to map the Last Glacial Maximum (LGM)
configuration of the southern and central parts of the Antarctic Peninsula Ice Sheet, and to …

Observations of relative sea-level (RSL) change in Great Britain since 16kyr BP and models
of post-glacial isostatic adjustment provide constraints on reconstructions of the British and …

Marine and terrestrial geological and marine geophysical data that constrain deglaciation
since the Last Glacial Maximum (LGM) of the sector of the West Antarctic Ice Sheet (WAIS) …

A reconstruction of the Antarctic Ice Sheet at the Last Glacial Maximum (LGM), constrained
by geologic data, shows expansion across continental shelves accompanied by little inland …