Effects of Climatic Perturbations on the Surface-Ablation Regime of the Greenland Ice Sheet, West Greenland [PDF]
W. Ambach
openalex +1 more source
Algae Drive Enhanced Darkening of Bare Ice on the Greenland Ice Sheet
Surface ablation of the Greenland ice sheet is amplified by surface darkening caused by light‐absorbing impurities such as mineral dust, black carbon, and pigmented microbial cells.
M. Stibal+17 more
semanticscholar +1 more source
Accelerating growth of Sermilik Delta, Greenland (1987–2022), driven by increasing runoff
By mapping delta shorelines and accounting for the impact of tides, we show that Sermilik Delta, southwest Greenland, has expanded >26 km2 since 1987 at an accelerating rate. We attribute delta growth to increasing meltwater runoff. The lack of correlation with ice velocity suggests a readily accessible store of sediments.
Rebecca Crick+2 more
wiley +1 more source
Complex motion of Greenland Ice Sheet outlet glaciers with basal temperate ice. [PDF]
Law R+5 more
europepmc +1 more source
Ice flow around large obstacles as indicated by basal ice exposed at the margin of the Greenland ice sheet [PDF]
Peter Knight+2 more
openalex +1 more source
European Temperature Extremes Under Different AMOC Scenarios in the Community Earth System Model
Abstract Recent simulations using the Community Earth System Model (CESM) indicate that a tipping event of the Atlantic Meridional Overturning Circulation (AMOC) would cause Europe to cool by several degrees. This AMOC tipping event was found under constant pre‐industrial greenhouse gas forcing, while global warming likely limits this AMOC‐induced ...
René M. van Westen+1 more
wiley +1 more source
Interactions of Fungi and Algae from the Greenland Ice Sheet. [PDF]
Perini L+9 more
europepmc +1 more source
Response of the Energy Balance on the Margin of the Greenland Ice Sheet to Temperature Changes [PDF]
Roger J. Braithwaite, Ole Β. Olesen
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Interpreting Ice Anisotropy of Greenland's Fastest Outlet Glacier Using Basal Icequakes
Abstract Ice anisotropy can have significant impact on ice rheology and flow dynamics. However, a lack of in situ measurements limits the validation and incorporation of anisotropy, so most ice flow models assume isotropic ice. Especially observations of anisotropy in fast‐flowing ice streams are scarce.
A. Nap+6 more
wiley +1 more source
Decreasing surface albedo signifies a growing importance of clouds for Greenland Ice Sheet meltwater production. [PDF]
Ryan JC+6 more
europepmc +1 more source