. With the aim of studying the recent Greenland ice sheet (GrIS) surface mass balance (SMB) decrease relative to the last century, we have forced the regional climate MAR (Modele Atmospherique Regional; version 3.5.2) model with the ERA-Interim (ECMWF ...
X. Fettweis +8 more
semanticscholar +1 more source
Improved retrieval of land ice topography from CryoSat-2 data and its impact for volume-change estimation of the Greenland Ice Sheet [PDF]
A new methodology for retrieval of glacier and ice sheet elevations and elevation changes from CryoSat-2 data is presented. Surface elevations and elevation changes determined using this approach show significant improvements over ESA's publicly ...
Forsberg, René +3 more
core +2 more sources
Rapid Basal Channel Growth Beneath Greenland's Longest Floating Ice Shelf
Nioghalvfjerdsfjorden Glacier (N79) is one of the two main outlets for Greenland's largest ice stream, the Northeast Greenland Ice Stream, and is the more stable of the two, with no calving front retreat expected in the near future. Using a novel surface
Ash Narkevic, Bea Csatho, Toni Schenk
doaj +1 more source
Significance The recent deglaciation of Greenland is a response to both oceanic and atmospheric forcings. From 2000 to 2010, ice loss was concentrated in the southeast and northwest margins of the ice sheet, in large part due to the increasing discharge ...
M. Bevis +13 more
semanticscholar +1 more source
Impact of ocean stratification on submarine melting of a major Greenland outlet glacier [PDF]
Submarine melting is an important balance term for tidewater glaciers1,2 and recent observations point to a change in the submarine melt rate as a potential trigger for the widespread acceleration of outlet glaciers in Greenland3-5.
Claudia Cenedese +6 more
core +1 more source
Sensitivity of a Greenland ice sheet model to atmospheric forcing fields [PDF]
International audiencePredicting the climate for the future and how it will impact ice sheet evolution requires coupling ice sheet models with climate models.
Fettweis, X. +8 more
core +3 more sources
East Greenland Ice Sheet retreat history from Scoresby Sund and Storstrømmen Glacier during the last deglaciation [PDF]
The lack of geological constraints on past ice-sheet change in marine-based sectors of the Greenland Ice Sheet (GrIS) following the Last Glacial Maximum limits our ability to assess (1) the drivers of ice-sheet change, and (2) the performance of ice ...
J. T. H. Anderson +9 more
doaj +1 more source
Dark zone of the Greenland Ice Sheet controlled by distributed biologically-active impurities
Albedo—a primary control on surface melt—varies considerably across the Greenland Ice Sheet yet the specific surface types that comprise its dark zone remain unquantified.
J. Ryan +7 more
semanticscholar +1 more source
On the recent contribution of the Greenland ice sheet to sea level change
. We assess the recent contribution of the Greenland ice sheet (GrIS) to sea level change. We use the mass budget method, which quantifies ice sheet mass balance (MB) as the difference between surface mass balance (SMB) and solid ice discharge across the
M. Broeke +7 more
semanticscholar +1 more source
Seasonal to decadal variability in ice discharge from the Greenland Ice Sheet.
Rapid changes in thickness and velocity have been observed at many marine-terminating glaciers in Greenland, impacting the volume of ice they export, or discharge, from the ice sheet.
M. King +6 more
semanticscholar +1 more source

