Results 81 to 90 of about 96,608 (241)
Peak refreezing in the Greenland firn layer under future warming scenarios
Greenland firn, the layer of compressed snow that today covers 90% of the ice sheet, currently retains half of the meltwater through refreezing. Here the authors use climate simulations to predict that refreezing in Greenland firn could peak at around ...
Brice Noël +4 more
doaj +1 more source
The Programme for Monitoring of the Greenland Ice Sheet (PROMICE) provides surface meteorological and glaciological measurements from widespread on-ice automatic weather stations since mid-2007.
Adrien Wehrlé +4 more
doaj +1 more source
Modelling snow accumulation on Greenland in Eemian, glacial inception, and modern climates in a GCM [PDF]
Changing climate conditions on Greenland influence the snow accumulation rate and surface mass balance (SMB) on the ice sheet and, ultimately, its shape.
G. Krinner +3 more
core +3 more sources
MIS-11 duration key to disappearance of the Greenland ice sheet [PDF]
Palaeo data suggest that Greenland must have been largely ice free during Marine Isotope Stage 11 (MIS-11). However, regional summer insolation anomalies were modest during this time compared to MIS-5e, when the Greenland ice sheet likely lost less ...
Calov, Reinhard +4 more
core +3 more sources
. Understanding the role of atmospheric circulation anomalies on the surface mass balance of the Greenland ice sheet (GrIS) is fundamental for improving estimates of its current and future contributions to sea level rise.
M. Tedesco, X. Fettweis
semanticscholar +1 more source
Recent Advances in Our Understanding of the Role of Meltwater in the Greenland Ice Sheet System [PDF]
Nienow, Sole and Cowton’s Greenland research has been supported by a number of UK NERC research grants (NER/O/S/2003/00620; NE/F021399/1; NE/H024964/1; NE/K015249/1; NE/K014609/1) and Slater has been supported by a NERC PhD studentshipPurpose of the ...
A Igneczi +103 more
core +3 more sources
The Greenland ice sheet has been losing mass in response to increased surface melting (Khan et al. 2015; van den Broeke et al. 2017) as well as discharge of ice from marine terminating outlet glaciers (van den Broeke et al. 2009; Box et al. 2018). Marine
Jonas K Andersen +17 more
doaj +1 more source
Greenland Ice Sheet surface melt amplified by snowline migration and bare ice exposure
Greenland’s snowline exhibits large fluctuations and is a primary amplifier of ice sheet surface melt and runoff. Greenland Ice Sheet mass loss has recently increased because of enhanced surface melt and runoff.
J. Ryan +9 more
semanticscholar +1 more source
The Greenland-Ice-Sheet evolution over the last 24 000 years: insights from model simulations evaluated against ice-extent markers [PDF]
Continental ice sheets retain a long-term memory stored in their geometry and thermal properties. In Greenland, this creates a disequilibrium with the present climate, as the ice sheet is still adjusting to past changes that occurred over millennial ...
T. P. M. Leger +6 more
doaj +1 more source
Monitoring of the Greenland ice sheet using a broadband seismometer network: the GLISN project
Global climate change is currently causing melting of the Greenland ice sheet. Recently, a new type of seismic event, referred to as a "glacial earthquake", has been recognized.
Genti Toyokuni +7 more
doaj +1 more source

