Results 91 to 100 of about 662,315 (337)

ISMIP6 Antarctica: a multi-model ensemble of the Antarctic ice sheet evolution over the 21st century

The Cryosphere, 2020
. Ice flow models of the Antarctic ice sheet are commonly used to simulate its future evolution in response to different climate scenarios and assess the mass loss that would contribute to future sea level rise.
H. Seroussi, S. Nowicki, A. Payne, H. Goelzer, W. Lipscomb, A. Abe‐Ouchi, Cécile Agosta, T. Albrecht, X. Asay-Davis, A. Barthel, R. Calov, R. Cullather, C. Dumas, B. Galton-Fenzi, R. Gladstone, N. Golledge, J. Gregory, R. Greve, T. Hattermann, M. Hoffman, A. Humbert, P. Huybrechts, N. Jourdain, T. Kleiner, E. Larour, G. Leguy, D. Lowry, C. M. Little, Mathieu Morlighem, F. Pattyn, T. Pelle, S. Price, A. Quiquet, R. Reese, N. Schlegel, A. Shepherd, E. Simon, Robin S. Smith, F. Straneo, Sainan Sun, L. Trusel, Jonas Van Breedam, R. V. D. van de Wal, R. Winkelmann, Chen Zhao, Tong Zhang, T. Zwinger   +46 more
semanticscholar   +1 more source

PLISMIP-ANT, an ice-sheet model intercomparison project [PDF]

, 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.
Abe-Ouchi, A., Bernales, J., Boer, B. de, Dolan, A. M., Gasson, E., Goelzer, H., Golledge, N. R., Huybrechts, P., Lohmann, G., Rogozhina, I., Saito, F., Sutter, J., Wal, R. S. W. van de   +12 more
core   +1 more source

Stabilization of Miscible Aqueous Phases via Diffusion‐Controlled Multifunctional Nanoparticle‐Ligand Complexation

Advanced Functional Materials, EarlyView.
This study presents a versatile approach to harnessing miscible aqueous domains, enabling liquid‐in‐liquid compartmentalization using a barrier formed in situ rather than bulk immiscibility. The barrier forms upon the complexation of multifunctional nanoparticles and ligands at the contact boundary of aqueous phases.
Seyyed Alireza Hashemi, Mahyar Panahi‐Sarmad, Ahmadreza Ghaffarkhah, Vahid Rad, Masoud Soroush, Thomas P. Russell, Orlando J. Rojas, Mohammad Arjmand   +7 more
wiley   +1 more source

Modeling the Cordilleran Ice Sheet [PDF]

Géographie physique et Quaternaire, 2007
A time-dependent ice flow model is used to provide detailed reconstructions of ice growth and retreat for the southern portion of the Late Wisconsinan Cordilleran Ice Sheet. The two-dimensional, time-dependent model provides ice surface elevations and flow directions at a grid spacing of 15 km.
openaire   +1 more source

The Grounding of an Ice Shelf in the Central Arctic Ocean: A Modeling Experiment [PDF]

, 2003
A numerical ice sheet model was used in a first test towards evaluating the hypothesis that, during a period of large-scale glaciation, an ice shelf emanating from the Barents/Kara Seas grounded across parts of the Lomonosov Ridge to a depth of around ...
Jakobsson, Martin, Paton, Mark, Siegert, M   +2 more
core   +1 more source

Combustion of available fossil-fuel resources sufficient to eliminate the Antarctic Ice Sheet [PDF]

, 2015
The Antarctic Ice Sheet stores water equivalent to 58 m in global sea-level rise. We show in simulations using the Parallel Ice Sheet Model that burning the currently attainable fossil fuel resources is sufficient to eliminate the ice sheet.
Aschwanden, Bueler, Bueler, Caldeira, Dutton, Eby, Favier, Feldmann, Frieler, Goodwin, Joughin, Li, Lingle, Mengel, Payne, Pollard, Ridley, Rignot, Robinson, Simmons, Uotila, Weertman, Winkelmann, Zickfeld   +23 more
core   +5 more sources

Scalable Polyelectrolyte Complex‐Based Sorbent With Hourly Sorption−Desorption Cycles for Multicyclic Atmospheric Water Harvesting in Arid Environments

Advanced Functional Materials, EarlyView.
A polyelectrolyte complex‐based sorbent is produced by scalable, environmentally benign aqueous phase inversion. Its porous, LiCl‐ and GO‐integrated architecture enables hourly adsorption−desorption cycles at low relative humidity (RH < 30%). A large‐scale prototype achieves multicyclic, solar‐driven atmospheric water harvesting of 1.37 L kg−1 day−1 ...
Seung‐Hwan Oh, Incheol Heo, Won Cheol Yoo, Soo‐Hyung Choi   +3 more
wiley   +1 more source

Interactive coupling of a Greenland ice sheet model in NorESM2 [PDF]

Geoscientific Model Development
On the backdrop of observed accelerating ice sheet mass loss over the last few decades, there is growing interest in the role of ice sheet changes in global climate projections.
H. Goelzer, P. M. Langebroek, A. Born, S. Hofer, S. Hofer, K. Haubner, M. Petrini, G. Leguy, W. H. Lipscomb, K. Thayer-Calder   +9 more
doaj   +1 more source

On the importance of the albedo parameterization for the mass balance of the Greenland ice sheet in EC-Earth [PDF]

The Cryosphere, 2017
The albedo of the surface of ice sheets changes as a function of time due to the effects of deposition of new snow, ageing of dry snow, bare ice exposure, melting and run-off.
M. M. Helsen, R. S. W. van de Wal, T. J. Reerink, R. Bintanja, M. S. Madsen, S. Yang, Q. Li, Q. Zhang   +7 more
doaj   +1 more source

Ocean–Ice Sheet Coupling in the Totten Glacier Area, East Antarctica: Analysis of the Feedbacks and Their Response to a Sudden Ocean Warming

Geosciences, 2023
We coupled together high-resolution versions of the ocean–sea ice model NEMO and the ice sheet model BISICLES configured to the Totten Glacier area and ran a series of simulations over the recent past (1995–2014) and under warming conditions (2081–2100 ...
Guillian Van Achter, Thierry Fichefet, Hugues Goosse, Charles Pelletier, Konstanze Haubner, Frank Pattyn   +5 more
doaj   +1 more source