Millennial-scale migration of the frozen/melted basal boundary, western Greenland ice sheet
The geometry and thermal structure of western Greenland ice sheet are known to have undergone relatively substantial change over the Holocene. Evolution of the frozen and melted fractions of the bed associated with the ice-sheet retreat over this time ...
Aidan Stansberry +3 more
doaj +1 more source
Investigations of the time-dependent behavior of marine ice sheets and their sensitivity to basal conditions require numerical models because existing theoretical analyses focus only on steady-state configurations primarily with a power-law basal shear ...
Olga Sergienko, Marianne Haseloff
doaj +1 more source
Experimental protocol for sea level projections from ISMIP6 stand-alone ice sheet models [PDF]
Projection of the contribution of ice sheets to sea level change as part of the Coupled Model Intercomparison Project Phase 6 (CMIP6) takes the form of simulations from coupled ice sheet–climate models and stand-alone ice sheet models, overseen by the ...
S. Nowicki +37 more
doaj +1 more source
Reply to “Basal buoyancy and fast-moving glaciers: in defense of analytic force balance” by C. J. van der Veen (2016) [PDF]
Two approaches to ice-sheet modeling are available. Analytical modeling is the traditional approach (Van der Veen, 2016). It solves the force (momentum), mass, and energy balances to obtain three-dimensional solutions over time, beginning with the ...
T. J. Hughes, T. J. Hughes
doaj +1 more source
The influence of inter-annual temperature variability on the Greenland Ice Sheet volume
The Greenland Ice Sheet has become an increasingly larger contributor to sea level rise in the past two decades and is projected to continue to lose mass.
Mikkel Lauritzen +5 more
doaj +1 more source
PISM-LakeCC: Implementing an adaptive proglacial lake boundary in an ice sheet model [PDF]
During the Late Pleistocene and Holocene retreat of paleo-ice sheets in North America and Europe, vast proglacial lakes existed along the land terminating margins.
S. Hinck +6 more
doaj +1 more source
Nonlinear response of the Antarctic Ice Sheet to late Quaternary sea level and climate forcing [PDF]
Antarctic ice volume has varied substantially during the late Quaternary, with reconstructions suggesting a glacial ice sheet extending to the continental shelf break and interglacial sea level highstands of several meters.
M. Tigchelaar +5 more
doaj +1 more source
Simulating the Holocene deglaciation across a marine-terminating portion of southwestern Greenland in response to marine and atmospheric forcings [PDF]
Numerical simulations of the Greenland Ice Sheet (GrIS) over geologic timescales can greatly improve our knowledge of the critical factors driving GrIS demise during climatically warm periods, which has clear relevance for better predicting GrIS behavior
J. K. Cuzzone +4 more
doaj +1 more source
Pre-LGM Northern Hemisphere ice sheet topography [PDF]
We here reconstruct the paleotopography of Northern Hemisphere ice sheets during the glacial maxima of marine isotope stages (MIS) 5b and 4.We employ a combined approach, blending geologically based reconstruction and numerical modeling, to arrive at ...
J. Kleman +4 more
doaj +1 more source
Ice mass loss sensitivity to the Antarctic ice sheet basal thermal state
This study uses ice sheet modeling experiments to show that thawing portions of the Antarctic ice sheet bed can increase century-scale mass loss, particularly in the Wilkes and Enderby Land regions of East Antarctica.
Eliza J. Dawson +4 more
doaj +1 more source

