Vertical land motion (VLM) from past and ongoing glacial changes can amplify or mitigate
ongoing relative sea level change. We present a high‐resolution VLM model for the wider …

Rapid regional warming in the Antarctic Peninsula has led to the significant retreat and
eventual collapse of several major ice shelves since the 1970s, triggering the subsequent …

Crustal motion generated by rapid ice‐mass loss from Earth's glaciers and ice sheets has
previously been considered in Global Navigational Satellite System (GNSS) analyses and …

The vertical movement of the Earth's surface is the result of a number of internal processes
in the solid Earth, tidal forces and mass redistribution in the atmosphere, oceans, terrestrial …

Three sensitivity experiments using an Ocean Atmosphere General Circulation Model
(OAGCM) are conducted to simulate the climate impact of precession. The relative …

In this study, we focus on improved constraint of the glacial isostatic adjustment (GIA) signal
at present-day, and its role as a contributor to present-day sea level budgets. The main study …

The effect of regional ocean loading on predicted rates of crustal uplift and gravitational
change due to glacial isostatic adjustment (GIA) is determined for Antarctica. The effect is …

The geodetic rates for the gravity variation and vertical uplift in polar regions subject to past
and present-day ice-mass changes (PDIMCs) provide important insight into the rheological …

Mass loss from glaciers and ice caps represents the largest terrestrial component of current
sea level rise. However, our understanding of how the processes governing mass loss will …

Melting glaciers, ice caps and ice sheets have made an important contribution to sea-level
rise through the last century. Self-attraction and loading effects driven by shrinking ice …