Higher boreal summer insolation in the early to middle Holocene drove thousands of years of summer warming across the Arctic. Modern-day warming has distinctly different causes …
Abstract The Greenland ice sheet (GrIS) is a growing contributor to global sea-level rise 1, with recent ice mass loss dominated by surface meltwater runoff 2, 3. Satellite observations …
Cold regions, including high-latitude and high-altitude landscapes, are experiencing profound environmental changes driven by global warming. With the advance of earth …
M Hörhold, T Münch, S Weißbach, S Kipfstuhl, J Freitag… - Nature, 2023 - nature.com
Abstract The Greenland Ice Sheet has a central role in the global climate system owing to its size, radiative effects and freshwater storage, and as a potential tipping point. Weather …
Surface meltwater runoff dominates present-day mass loss from the Greenland Ice Sheet. In Greenland's interior, porous firn can limit runoff by retaining meltwater unless perched low …
Meteorological Drivers and Large-Scale Climate Forcing of West Antarctic Surface Melt in: Journal of Climate Volume 32 Issue 3 (2019) Jump to Content Jump to Main Navigation …
A porous layer of multi-year snow known as firn covers the Greenland-ice-sheet interior. The firn layer buffers the ice-sheet contribution to sea-level rise by retaining a fraction of summer …
We assess temperature and moisture transport in and around the Antarctic Peninsula (AP) associated with atmospheric blocking over two domains, one located to the west (150–90° …
K Kawakami, Y Iizuka, M Sasage… - Journal of …, 2023 - Wiley Online Library
Arctic warming has accelerated surface melting even in the highland areas of the Greenland ice sheet (GrIS). Understanding the relationship between climate and surface melting is …