Differences between the last two glacial maxima and implications for ice-sheet, δ18O, and sea-level reconstructions
Studies of past glacial cycles yield critical information about climate and sea-level (ice-
volume) variability, including the sensitivity of climate to radiative change, and impacts of …
volume) variability, including the sensitivity of climate to radiative change, and impacts of …
The GRISLI ice sheet model (version 2.0): calibration and validation for multi-millennial changes of the Antarctic ice sheet
In this paper, we present the GRISLI (Grenoble ice sheet and land ice) model in its newest
revision (version 2.0). Whilst GRISLI is applicable to any given ice sheet, we focus here on …
revision (version 2.0). Whilst GRISLI is applicable to any given ice sheet, we focus here on …
Numerical reconstructions of the Northern Hemisphere ice sheets through the last glacial-interglacial cycle
S Charbit, C Ritz, G Philippon, V Peyaud… - Climate of the …, 2007 - cp.copernicus.org
A 3-dimensional thermo-mechanical ice-sheet model is used to simulate the evolution of the
Northern Hemisphere ice sheets through the last glacial-interglacial cycle. The ice-sheet …
Northern Hemisphere ice sheets through the last glacial-interglacial cycle. The ice-sheet …
Quantifying the uncertainty in the Eurasian ice-sheet geometry at the Penultimate Glacial Maximum (Marine Isotope Stage 6)
OG Pollard, NLM Barlow, L Gregoire… - The Cryosphere …, 2023 - tc.copernicus.org
North Sea Last Interglacial sea level is sensitive to the fingerprint of mass loss from polar ice
sheets. However, the signal is complicated by the influence of glacial isostatic adjustment …
sheets. However, the signal is complicated by the influence of glacial isostatic adjustment …
Assimilation de données pour l'initialisation et l'estimation de paramètres d'un modèle d'évolution de calotte polaire
B Bonan - 2013 - theses.hal.science
L'évolution des calottes polaires est régie à la fois par une dynamique d'écoulement
complexe et par des mécanismes tel le glissement à la base, la température de la glace ou …
complexe et par des mécanismes tel le glissement à la base, la température de la glace ou …
Reconstruction de la calotte polaire du Groenland au cours du dernier cycle glaciaire-interglaciaire à partir de l'association de la modélisation numérique 3D et des …
A Quiquet - 2012 - theses.hal.science
La calotte polaire du Groenland retient dans ses glaces une contribution potentielle au
niveau des mers de 7, 3 mètres. Alors que des changements importants sont observés à …
niveau des mers de 7, 3 mètres. Alors que des changements importants sont observés à …
[PDF][PDF] Long-term safety of a planned geological repository for spent nuclear fuel in Forsmark, Sweden and Olkiluoto, Finland
The following report constitutes a second and final phase of a study reconstructing the
Eurasian ice sheet during the peak Saalian glaciation, 140 000 years ago, by climate-and …
Eurasian ice sheet during the peak Saalian glaciation, 140 000 years ago, by climate-and …
Reconstructing with numerical Ice Sheet Models the post-LGM decay of the Eurasian Ice Sheets: data-model comparison and focus on the Storfjorden (Svalbard) ice …
M Petrini - 2017 - arts.units.it
The challenge of reconstructing the growth and decay of palaeo-ice sheets represents a
critical task to better understand mechanisms of global climate change and associated sea …
critical task to better understand mechanisms of global climate change and associated sea …
The Cryosphere and Sea Level
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Account Menu Find a journal Publish with us Track your research Search Cart Book cover …
Account Menu Find a journal Publish with us Track your research Search Cart Book cover …
Rôle des calottes glaciaires dans le système climatique: Analyse des interactions entre un modèle de calotte de glace Antarctique et un modèle de climat
G Philippon - 2007 - theses.hal.science
Le système climatique fait intervenir plusieurs composantes qui interagissent entre elles
avec des constantes de temps très différentes, dont l'atmosphère, l'hydrosphère, la …
avec des constantes de temps très différentes, dont l'atmosphère, l'hydrosphère, la …