Results 11 to 20 of about 306,492 (342)

Coupling framework (1.0) for the PISM (1.1.4) ice sheet model and the MOM5 (5.1.0) ocean model via the PICO ice shelf cavity model in an Antarctic domain [PDF]

open access: yesGeoscientific Model Development, 2021
The past and future evolution of the Antarctic Ice Sheet is largely controlled by interactions between the ocean and floating ice shelves. To investigate these interactions, coupled ocean and ice sheet model configurations are required.
M. Kreuzer   +8 more
doaj   +2 more sources

High climate model dependency of Pliocene Antarctic ice-sheet predictions

open access: yesNature Communications, 2018
Ice sheet models forced by climate model output indicate ice-sheet retreat during the Pliocene, yet concerns remain regarding potential model bias. Here, the authors present results from the Pliocene Ice-sheet Modelling Intercomparison Project, and show ...
Aisling M. Dolan   +4 more
doaj   +2 more sources

Data assimilation and prognostic whole ice sheet modelling with the variationally derived, higher order, open source, and fully parallel ice sheet model VarGlaS [PDF]

open access: yesThe Cryosphere, 2013
We introduce a novel, higher order, finite element ice sheet model called VarGlaS (Variational Glacier Simulator), which is built on the finite element framework FEniCS.
D. J. Brinkerhoff, J. V. Johnson
doaj   +2 more sources

Ice sheet model dependency of the simulated Greenland Ice Sheet in the mid-Pliocene [PDF]

open access: yesClimate of the Past, 2015
The understanding of the nature and behavior of ice sheets in past warm periods is important for constraining the potential impacts of future climate change.
S. J. Koenig   +12 more
doaj   +2 more sources

Hysteresis of the Antarctic Ice Sheet With a Coupled Climate‐Ice‐Sheet Model

open access: yesGeophysical Research Letters
The stability of the Antarctic ice sheet under different fixed CO2 levels and orbital configurations is explored using a coupled climate‐ice sheet model, starting from either a pre‐industrial ice sheet or an ice‐free, isostatically rebounded geometry ...
G. Leloup   +4 more
doaj   +5 more sources

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

open access: yesGeoscientific Model Development, 2014
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). End-member
J. G. Fyke, W. J. Sacks, W. H. Lipscomb
doaj   +4 more sources

Marine ice sheet experiments with the Community Ice Sheet Model [PDF]

open access: yesThe Cryosphere, 2021
Ice sheet models differ in their numerical treatment of dynamical processes. Simulations of marine-based ice are sensitive to the choice of Stokes flow approximation and basal friction law and to the treatment of stresses and melt rates near the ...
G. R. Leguy   +2 more
doaj   +1 more source

A Gaussian process emulator for simulating ice sheet–climate interactions on a multi-million-year timescale: CLISEMv1.0 [PDF]

open access: yesGeoscientific Model Development, 2021
On multi-million-year timescales, fully coupled ice sheet–climate simulations are hampered by computational limitations, even at coarser resolutions and when using asynchronous coupling schemes.
J. Van Breedam   +2 more
doaj   +1 more source

The GRISLI-LSCE contribution to the Ice Sheet Model Intercomparison Project for phase 6 of the Coupled Model Intercomparison Project (ISMIP6) – Part 2: Projections of the Antarctic ice sheet evolution by the end of the 21st century [PDF]

open access: yesThe Cryosphere, 2021
The Antarctic ice sheet's contribution to global sea level rise over the 21st century is of primary societal importance and remains largely uncertain as of yet.
A. Quiquet, C. Dumas
doaj   +1 more source

The GRISLI-LSCE contribution to the Ice Sheet Model Intercomparison Project for phase 6 of the Coupled Model Intercomparison Project (ISMIP6) – Part 1: Projections of the Greenland ice sheet evolution by the end of the 21st century [PDF]

open access: yesThe Cryosphere, 2021
Polar amplification will result in amplified temperature changes in the Arctic with respect to the rest of the globe, making the Greenland ice sheet particularly vulnerable to global warming. While the ice sheet has been showing an increased mass loss in
A. Quiquet, C. Dumas
doaj   +1 more source

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