Modeling the influence of Greenland ice sheet melting on the Atlantic meridional overturning circulation during the next millennia

By E. Driesschaert, T. Fichefet, Hugues Goosse, P. Huybrechts, I. Janssens, A. Mouchet, G. Munhoven, V. Brovkin, S. Weber. 2007

211 citations recorded by the source corpus.

Subfields: Atmospheric Science

View Paper: https://www.semanticscholar.org/paper/5834c4eb8f7ff34a0896aa1f1e9a28015b4c0376

How researchers see this paper

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In Atmospheric Science

1. Hans Renssen
2. Hugues Goosse
3. A. Timmermann
4. D. Roche
5. A. Montety
6. Jürgen Kurths
7. Frank M. Selten
8. M. Mann

Citations in the corpus

• An elastic-viscous-plastic sea ice model formulated on Arakawa B and C grids (2009, methodology): “…1999), and MOM3 (Modular Ocean Model, version 3, Hofmann and Morales Maqueda (2006)), as well as to Earth system models of intermediate complexity CLIMBER3α (Montoya et al., 2005) and LOVECLIM (Driesschaert et al., 2007), and to the climate general circulation model IPSL-CM4 (Marti et al., 2008).”
• Reconstructing surface temperature changes over the past 600 years using climate model simulations with data assimilation (2010, background): “LOVECLIM [ Driesschaert et al. , 2007] is a three ‐ dimensional Earth system model of intermediate complexity that includes representations of the atmosphere, the ocean and sea ice, the land surface (including vegetation), the ice sheets, and the carbon cycle.”
• Deconstructing the Last Glacial termination: the role of millennial and orbital-scale forcings (2011, methodology): “Our goal is to simulate the Last Glacial Termination using an Earth system model of intermediate complexity, LOVECLIM, and to address the following questions: What forcings are needed to reproduce the dominant climate and biogeochemical features of the Last Glacial Termination?”
• Description of the Earth system model of intermediate complexity LOVECLIM version 1.2 (2010, methodology): “More recently, two additional components were added (Driesschaert et al., 2007): the ocean carbon cycle model LOCH (Mouchet and François, 1996) and the ice sheet model AGISM (Huybrechts, 2002).”
• Interacting tipping elements increase risk of climate domino effects under global warming (2020, methodology): “Increasing freshwater input from enhanced melting of the Greenland Ice Sheet can lead to a weakening of the AMOC, as supported by palaeoclimate evidence as well as modelling studies (Driesschaert et al., 2007; Jungclaus et al., 2006; Rahmstorf et al., 2005).”
• A systematic study of the impact of freshwater pulses with respect to different geographical locations (2010, methodology): “We here only use the atmosphere–ocean–vegetation modules (equivalent to ECBilt–CLIO–VECODE version 3), a model already used in studies on the Holocene (Renssen et al. 2005), the last and the next millennium (Goosse et al. 2005; Driesschaert et al. 2007) or the LGM (Roche et al. 2007).”