ISMIP6 Antarctica: a multi-model ensemble of the Antarctic ice sheet evolution over the 21st century
Ice flow models of the Antarctic ice sheet are commonly used to simulate its future evolution
in response to different climate scenarios and inform on the mass loss that would contribute …
in response to different climate scenarios and inform on the mass loss that would contribute …
[HTML][HTML] The future sea-level contribution of the Greenland ice sheet: a multi-model ensemble study of ISMIP6
The Greenland ice sheet is one of the largest contributors to global mean sea-level rise
today and is expected to continue to lose mass as the Arctic continues to warm. The two …
today and is expected to continue to lose mass as the Arctic continues to warm. The two …
Projecting Antarctica's contribution to future sea level rise from basal ice shelf melt using linear response functions of 16 ice sheet models (LARMIP-2)
The sea level contribution of the Antarctic ice sheet constitutes a large uncertainty in future
sea level projections. Here we apply a linear response theory approach to 16 state-of-the-art …
sea level projections. Here we apply a linear response theory approach to 16 state-of-the-art …
initMIP-Antarctica: an ice sheet model initialization experiment of ISMIP6
Ice sheet numerical modeling is an important tool to estimate the dynamic contribution of the
Antarctic ice sheet to sea level rise over the coming centuries. The influence of initial …
Antarctic ice sheet to sea level rise over the coming centuries. The influence of initial …
Evolution of the Antarctic Ice Sheet over the next three centuries from an ISMIP6 model ensemble
Abstract The Ice Sheet Model Intercomparison Project for CMIP6 (ISMIP6) is the primary
effort of CMIP6 (Coupled Model Intercomparison Project–Phase 6) focusing on ice sheets …
effort of CMIP6 (Coupled Model Intercomparison Project–Phase 6) focusing on ice sheets …
Glacial-cycle simulations of the Antarctic Ice Sheet with the Parallel Ice Sheet Model (PISM)–Part 2: parameter ensemble analysis
Abstract The Parallel Ice Sheet Model (PISM) is applied to the Antarctic Ice Sheet over the
last two glacial cycles (≈ 210 000 years) with a resolution of 16 km. An ensemble of 256 …
last two glacial cycles (≈ 210 000 years) with a resolution of 16 km. An ensemble of 256 …
[HTML][HTML] Revisiting temperature sensitivity: how does Antarctic precipitation change with temperature?
With progressing global warming, snowfall in Antarctica is expected to increase, which could
counteract or even temporarily overcompensate increased ice-sheet mass losses caused by …
counteract or even temporarily overcompensate increased ice-sheet mass losses caused by …
Glacial isostatic adjustment and post-seismic deformation in Antarctica
This chapter reviews glacial isostatic adjustment (GIA) and post-seismic deformation in
Antarctica. It discusses numerical models and their inputs, and observations and inferences …
Antarctica. It discusses numerical models and their inputs, and observations and inferences …
Investigating similarities and differences of the penultimate and last glacial terminations with a coupled ice sheet–climate model
Glacial terminations are marked by a re-organisation of the different components of the
climate system. In particular, rapid ice sheet disintegration leads to multiple complex …
climate system. In particular, rapid ice sheet disintegration leads to multiple complex …
Assessment of the Greenland ice sheet–atmosphere feedbacks for the next century with a regional atmospheric model coupled to an ice sheet model
In the context of global warming, growing attention is paid to the evolution of the Greenland
ice sheet (GrIS) and its contribution to sea-level rise at the centennial timescale. Atmosphere …
ice sheet (GrIS) and its contribution to sea-level rise at the centennial timescale. Atmosphere …