Results 51 to 60 of about 407 (118)

A technique for generating consistent ice sheet initial conditions for coupled ice sheet/climate models [PDF]

open access: yesGeoscientific Model Development, 2013
Abstract. A transient technique for generating ice sheet preindustrial initial conditions for long-term coupled ice sheet/climate model simulations is developed and demonstrated over the Greenland ice sheet using the Community Earth System Model (CESM).
J. G. Fyke, W. J. Sacks, W. H. Lipscomb
openaire   +3 more sources

The impact of the North American glacial topography on the evolution of the Eurasian ice sheet over the last glacial cycle [PDF]

open access: yesClimate of the Past, 2016
Modeling studies have shown that the continental-scale ice sheets in North America and Eurasia in the last glacial cycle had a large influence on the atmospheric circulation and thus yielded a climate distinctly different from the present.
J. Liakka, M. Löfverström, F. Colleoni
doaj   +1 more source

Exposure age and ice-sheet model constraints on Pliocene East Antarctic ice sheet dynamics [PDF]

open access: yesNature Communications, 2015
AbstractThe Late Pliocene epoch is a potential analogue for future climate in a warming world. Here we reconstruct Plio-Pleistocene East Antarctic Ice Sheet (EAIS) variability using cosmogenic nuclide exposure ages and model simulations to better understand ice sheet behaviour under such warm conditions.
Yamane, Masako   +6 more
openaire   +2 more sources

Error sources in basal yield stress inversions for Jakobshavn Isbræ, Greenland, derived from residual patterns of misfit to observations

open access: yesJournal of Glaciology, 2017
The basal interface of glaciers is generally not directly observable. Geophysical inverse methods are therefore used to infer basal parameters from surface observations.
MARIJKE HABERMANN   +2 more
doaj   +1 more source

Influence of ice-sheet geometry and supraglacial lakes on seasonal ice-flow variability [PDF]

open access: yesThe Cryosphere, 2013
Supraglacial lakes play an important role in establishing hydrological connections that allow lubricating seasonal meltwater to reach the base of the Greenland Ice Sheet.
I. Joughin   +9 more
doaj   +1 more source

A Three-Dimensional Model of the Antarctic Ice Sheet [PDF]

open access: yesAnnals of Glaciology, 1988
A preliminary version of a three-dimensional ice-sheet model for later use in climate models, but excluding ice shelves and basal sliding, is presented and applied to the Antarctic ice sheet. In the model, the three-dimensional fields of velocity and temperature are calculated in the coupled mode, and the temperature equation is integrated for 150 000 ...
openaire   +2 more sources

A synthesis of the basal thermal state of the Antarctic ice sheet

open access: yesJournal of Glaciology
The basal thermal state of the Antarctic ice sheet (AIS)—whether the base is frozen or thawed—fundamentally underpins its flow and is an important factor in understanding its large-scale response to external forcings.
Owen Seiner   +3 more
doaj   +1 more source

The paradigm shift in Antarctic ice sheet modelling [PDF]

open access: yesNature Communications, 2018
The Antarctic ice sheet is one of the largest potential contributors to future sea level rise. Predicting its future behaviour using physically-based ice sheet models has been a bottleneck for the past decades, but major advances are ongoing.
openaire   +4 more sources

Machine-learning emulation of the modeled basal thermal state for Totten Glacier

open access: yesJournal of Glaciology
The basal thermal state of the Antarctic ice sheet strongly influences ice dynamics and mass balance. Although basal thermal states can be simulated using ice-sheet models, significant uncertainties persist, with poorly constrained geothermal heat flux ...
Junshun Wang   +3 more
doaj   +1 more source

The Greenland Ice Sheet Large Ensemble (GrISLENS): simulating the future of Greenland under climate variability [PDF]

open access: yesThe Cryosphere
The Greenland ice sheet has lost ice at an increasing pace over recent decades, driven by a combination of human-caused climate change and internal variability in the climate system.
V. Verjans   +8 more
doaj   +1 more source

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