Results 61 to 70 of about 662,315 (337)
Relative sea-level rise around East Antarctica during Oligocene glaciation [PDF]
During the middle and late Eocene (∼48-34 Myr ago), the Earth's climate cooled and an ice sheet built up on Antarctica. The stepwise expansion of ice on Antarcticainduced crustal deformation and gravitational perturbations around the continent.
Adam Klaus +73 more
core +2 more sources
. We use an observationally calibrated ice-sheet model to investigate the future trajectory of the Antarctic ice sheet related to uncertainties in the future balance between sub-shelf melting and ice discharge, on the one hand, and the surface mass ...
Violaine Coulon +6 more
semanticscholar +1 more source
. We introduce MPAS-Albany Land Ice (MALI) v6.0, a new variable-resolution land ice model that uses unstructured Voronoi grids on a plane or sphere.
M. Hoffman +9 more
semanticscholar +1 more source
. The Antarctic Ice Sheet will play a crucial role in the evolution of global mean sea-level as the climate warms. An interactively coupled climate and ice sheet model is needed to understand the impacts of ice—climate feedbacks during this evolution ...
Antony Siahaan +9 more
semanticscholar +1 more source
Observing and Modeling Ice Sheet Surface Mass Balance [PDF]
AbstractSurface 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. As ice sheet SMB varies highly across multiple scales of space (meters to hundreds of kilometers) and time (hourly ...
Jan T. M. Lenaerts +3 more
openaire +6 more sources
Соціально-правова та етична природа мусульманської сім‘ї [PDF]
Relative sea-level variations during the late Pleistocene can only be reconstructed with the knowledge of ice-sheet history. On the other hand, the knowledge of regional and global relative sea-level variations is necessary to learn about the changes in ...
B. de Boer +2 more
core +2 more sources
Representing grounding line migration in synchronous coupling between a marine ice sheet model and a z-coordinate ocean model [PDF]
Synchronous coupling is developed between an ice sheet model and a z-coordinate ocean model (the MITgcm). A previously-developed scheme to allow continuous vertical movement of the ice-ocean interface of a floating ice shelf (“vertical coupling”) is ...
arthern, robert +7 more
core +3 more sources
Experimental design for three interrelated marine ice sheet and ocean model intercomparison projects: MISMIP v. 3 (MISMIP +), ISOMIP v. 2 (ISOMIP +) and MISOMIP v. 1 (MISOMIP1) [PDF]
Coupled ice sheet–ocean models capable of simulating moving grounding lines are just becoming available. Such models have a broad range of potential applications in studying the dynamics of marine ice sheets and tidewater glaciers, from process studies ...
X. S. Asay-Davis +13 more
doaj +1 more source
Description and validation of the ice-sheet model Yelmo (version 1.0)
. We describe the physics and features of the ice-sheet model Yelmo, an open-source project intended for collaborative development. Yelmo is a thermomechanical model, solving for the coupled velocity and temperature solutions of an ice sheet ...
A. Robinson +5 more
semanticscholar +1 more source
GRANTSISM: An Excel™ ice sheet model for use in introductory Earth science courses [PDF]
GRANTISM (GReenland and ANTarctic Ice Sheet Model) is an educational Excel™ model introduced by Pattyn (2006). Here, GRANTISM is amended to simulate the Svalbard-Barents-Sea Ice Sheet during the Last Glacial Maximum, an analogue for the contemporary West
Gowan, Evan J. +6 more
core +2 more sources

