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All Outputs (9)

Late Holocene relative sea levels near Palmer Station, northern Antarctic Peninsula, strongly controlled by late Holocene ice-mass changes (2018)
Journal Article

Many studies of Holocene relative sea-level (RSL) changes across Antarctica assume that their reconstructions record uplift from glacial isostatic adjustment caused by the demise of the Last Glacial Maximum (LGM) ice sheets. However, recent analysis... Read More about Late Holocene relative sea levels near Palmer Station, northern Antarctic Peninsula, strongly controlled by late Holocene ice-mass changes.

Glacial Isostatic Adjustment modelling: historical perspectives, recent advances, and future directions (2018)
Journal Article

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 component of GIA is postglacial rebound, which specifically rel... Read More about Glacial Isostatic Adjustment modelling: historical perspectives, recent advances, and future directions.

The impact of lateral variations in lithospheric thickness on glacial isostatic adjustment in West Antarctica (2018)
Journal Article

Differences in predictions of Glacial Isostatic Adjustment (GIA) for Antarctica persist due to uncertainties in deglacial history and Earth rheology. The Earth models adopted in many GIA studies are defined by parameters that vary in the radial direc... Read More about The impact of lateral variations in lithospheric thickness on glacial isostatic adjustment in West Antarctica.