Results 1 to 10 of about 1,626,068 (395)

Simulating the Antarctic ice sheet in the late-Pliocene warm period: PLISMIP-ANT, an ice-sheet model intercomparison project [PDF]

The Cryosphere, 2015
In the context of future climate change, understanding the nature and behaviour of ice sheets during warm intervals in Earth history is of fundamental importance.
B. de Boer, A. M. Dolan, J. Bernales, E. Gasson, H. Goelzer, N. R. Golledge, J. Sutter, P. Huybrechts, G. Lohmann, I. Rogozhina, A. Abe-Ouchi, F. Saito, R. S. W. van de Wal   +12 more
doaj   +19 more sources

Experimental protocol for sea level projections from ISMIP6 stand-alone ice sheet models [PDF]

The Cryosphere, 2020
. 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, H. Goelzer, H. Seroussi, A. Payne, W. Lipscomb, A. Abe‐Ouchi, Cécile Agosta, P. Alexander, X. Asay-Davis, A. Barthel, T. Bracegirdle, R. Cullather, D. Felikson, X. Fettweis, J. Gregory, T. Hattermann, N. Jourdain, P. Kuipers Munneke, E. Larour, C. Little, Mathieu Morlighem, I. Nias, A. Shepherd, E. Simon, D. Slater, Robin S. Smith, F. Straneo, L. Trusel, M. R. van den Broeke, R. V. D. van de Wal   +29 more
semanticscholar   +2 more sources

Climatic Conditions for modelling the Northern Hemisphere ice sheets throughout the ice age cycle [PDF]

Climate of the Past, 2007
The ice sheet-climate interaction as well as the climatic response to orbital parameters and atmospheric CO₂ concentration are examined in order to drive an ice sheet model throughout an ice age cycle.
A. Abe-Ouchi, T. Segawa, F. Saito
doaj   +6 more sources

Antarctic ice sheet response to sudden and sustained ice-shelf collapse (ABUMIP)

Journal of Glaciology, 2020
Antarctica's ice shelves modulate the grounded ice flow, and weakening of ice shelves due to climate forcing will decrease their ‘buttressing’ effect, causing a response in the grounded ice.
Sainan Sun, F. Pattyn, E. Simon, T. Albrecht, S. Cornford, R. Calov, C. Dumas, F. Gillet‐Chaulet, H. Goelzer, N. Golledge, R. Greve, M. Hoffman, A. Humbert, Elise Kazmierczak, T. Kleiner, G. Leguy, W. Lipscomb, Daniel F. Martin, Mathieu Morlighem, S. Nowicki, D. Pollard, S. Price, A. Quiquet, H. Seroussi, Tanja Schlemm, J. Sutter, R. V. D. van de Wal, R. Winkelmann, Tong Zhang   +28 more
semanticscholar   +3 more sources

Observing and Modeling Ice Sheet Surface Mass Balance

Reviews of Geophysics, 2019
Surface mass balance (SMB) provides mass input to the surface of the Antarctic and Greenland Ice Sheets and therefore comprises an important control on ice sheet mass balance and resulting contribution to global sea level change.
Jan T M Lenaerts, Brooke Medley, Bert Wouters   +2 more
exaly   +2 more sources

Competing climate feedbacks of ice sheet freshwater discharge in a warming world. [PDF]

Nat Commun
Freshwater discharge from ice sheets induces surface atmospheric cooling and subsurface ocean warming, which are associated with negative and positive feedbacks respectively. However, uncertainties persist regarding these feedbacks’ relative strength and
Li D, DeConto RM, Pollard D, Hu Y.
europepmc   +2 more sources

Mass balance of the Greenland Ice Sheet from 1992 to 2018

Nature, 2019
The Imbie Team
exaly   +2 more sources

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

Geoscientific 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, P. Huybrechts, M. Crucifix   +2 more
doaj   +1 more source

Investigating the internal structure of the Antarctic ice sheet: the utility of isochrones for spatiotemporal ice-sheet model calibration [PDF]

The Cryosphere, 2021
Ice-sheet models are a powerful tool to project the evolution of the Greenland and Antarctic ice sheets and thus their future contribution to global sea-level changes. Testing the ability of ice-sheet models to reproduce the ongoing and past evolution of
J. Sutter, H. Fischer, O. Eisen, O. Eisen   +3 more
doaj   +1 more source

Growth and retreat of the last British–Irish Ice Sheet, 31 000 to 15 000 years ago: the BRITICE‐CHRONO reconstruction

Boreas, 2022
The BRITICE‐CHRONO consortium of researchers undertook a dating programme to constrain the timing of advance, maximum extent and retreat of the British–Irish Ice Sheet between 31 000 and 15 000 years before present. The dating campaign across Ireland and
C. Clark, J. Ely, R. Hindmarsh, S. Bradley, Á. Ignéczi, D. Fabel, C. Ó Cofaigh, R. Chiverrell, J. Scourse, S. Benetti, T. Bradwell, D. Evans, D. Roberts, M. Burke, S. L. Callard, A. Medialdea, M. Saher, D. Small, R. Smedley, E. Gasson, L. Gregoire, N. Gandy, A. Hughes, C. Ballantyne, M. Bateman, G. Bigg, J. Doole, D. Dove, G. Duller, Geraint T. H. Jenkins, S. Livingstone, S. Mccarron, S. Moreton, David Pollard, D. Praeg, H. Sejrup, K. V. van Landeghem, P. Wilson   +37 more
semanticscholar   +1 more source