Over the past decade, the Arctic has warmed by 0.75° C, far outpacing the global average,
while Antarctic temperatures have remained comparatively stable. As Earth approaches 2° …

Despite the increased recognition of the importance of images as a rich data source, the full
potential of images to advance tourism and hospitality knowledge, both conceptually and …

Abstract The Paris Agreement aims to limit global mean warming in the twenty-first century to
less than 2 degrees Celsius above preindustrial levels, and to promote further efforts to limit …

The reasons for concern framework communicates scientific understanding about risks in
relation to varying levels of climate change. The framework, now a cornerstone of the IPCC …

Mechanisms such as ice‐shelf hydrofracturing and ice‐cliff collapse may rapidly increase
discharge from marine‐based ice sheets. Here, we link a probabilistic framework for sea …

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 …

To predict the future contributions of the Antarctic ice sheets to sea-level rise, numerical
models use reconstructions of past ice-sheet retreat after the Last Glacial Maximum to tune …

Abstract The Antarctic Ice Sheet (AIS) is out of equilibrium with the current anthropogenic‐
enhanced climate forcing. Paleoenvironmental records and ice sheet models reveal that the …

Recent studies suggest that Antarctica has the potential to contribute up to~ 15 m of sea-
level rise over the next few centuries. The evolution of the Antarctic Ice Sheet is driven by a …

Ice sheet numerical modeling is an important tool to estimate the dynamic contribution of the
Antarctic ice sheet to sea level rise over the coming centuries. The influence of initial …