Kevin Fleming

TL;DR: In this paper, the eustatic component of relative sea-level change provides a measure of the amount of ice transferred between the continents and oceans during glacial cycles, which has been quantified for the period since the last glacial maximum by correcting observed sea level change for the glacio-hydro-isostatic contributions using realistic ice distribution and earth models.

TL;DR: In this paper, the authors combined geomorphological descriptions of changes in the extent of the Greenland Ice Sheet (GIS) with glacial-isostatic-adjustment models to reproduce the sea-level history of Greenland since the Last Glacial Maximum (LGM).

TL;DR: In this paper, the authors identify perceptions of two decision-making tools, which involve multi-hazard and multi-risk, based on the feedback from stakeholders, and find that interest in multirisk assessment is high but that its application remains hampered by the complexity of processes involved.

TL;DR: In this paper, a detailed knowledge of the thickness of the lithosphere in the north Atlantic is obtained using the seismic technique of S-receiver functions, with as yet unprecedented detail.

TL;DR: The new deglaciation history and GIA uplift estimates suggest that studies that use the Gravity Recovery and Climate Experiment satellite mission to infer present-day changes in the GrIS may have erroneously corrected for GIA and underestimated the mass loss by about 20 gigatons/year.