Results 1 to 10 of about 1,109 (131)
Increased oceanic heat transport plays a key role in the accelerated mass loss of Greenland’s marine‐terminating glaciers. The melt rate of major glaciers in Northeast Greenland (NEG) is controlled by ocean variability, in particular warm Atlantic ...
R. McPherson, C. Wekerle, T. Kanzow
semanticscholar +1 more source
Deep-water circulation in the northeast Atlantic during the mid- and Late Cretaceous
The Cretaceous ocean was significantly different from its modern counterpart due to its ice-free condition. Deep waters were primarily sourced by evaporation at the ocean surface, although their circulation pattern and bottom-current dynamics have been ...
Shan Liu +3 more
semanticscholar +1 more source
Using a large ensemble of simulations from the Polar Amplification Model Intercomparison Project (PAMIP) and Coupled Model Intercomparison Project Phase 6 (CMIP6), we compare the response of winter-mean precipitation and daily extremes across the North ...
Hao Yu +4 more
semanticscholar +1 more source
The interaction between ocean circulation and ice‐sheet dynamics plays a key role in the Quaternary climate. Compared with the surface and deep regions of the Atlantic Meridional Overturning Circulation (AMOC), the study of intermediate depths during key
P. Depuydt +4 more
semanticscholar +1 more source
While previous studies consistently suggest that North Atlantic Deep Water (NADW) was shallower at the Last Glacial Maximum (LGM) than at pre‐industrial, its strength is still controversial.
L. Menviel +6 more
semanticscholar +1 more source
During the past four decades significant decrease in Arctic sea ice and a dramatic ice mass loss of the Greenland Ice Sheet (GIS) has been coincident with global warming and an increase in atmospheric CO2.
Nicole Syring +6 more
semanticscholar +1 more source
The waters adjacent to the Nioghalvfjerdsbræ (79 North Glacier, 79NG) are influenced by Greenland Ice Sheet (GrIS) melt, sea-ice meltwater, and waters on the adjacent northeast Greenland shelf (NEGS).
A. Fransson +4 more
semanticscholar +1 more source
Stable Atlantic Deep Water Mass Sourcing on Glacial‐Interglacial Timescales
Increased deep ocean carbon storage is often invoked as the major sink for lower atmospheric CO2 concentrations during past ice ages. In order to improve the understanding of the changes in ocean dynamics facilitating such increased oceanic carbon ...
F. Pöppelmeier +5 more
semanticscholar +1 more source
The Amazon River plume, a barrier to animal dispersal in the Western Tropical Atlantic
The dispersal of marine organisms can be restricted by a set of isolation mechanisms including hard barriers or hydrological features. In the Western Atlantic Ocean, the Amazon River discharge has been shown to act as a biogeographical barrier ...
Everton Giachini Tosetto +3 more
semanticscholar +2 more sources
. Temperature in northeast Greenland is expected to rise at a faster rate than the global average as a consequence of anthropogenic climate change. Associated with this temperature rise, precipitation is also expected to increase as a result of increased
Lilian Schuster +3 more
semanticscholar +1 more source

