Space geodesy constrains ice age terminal deglaciation: The global ICE‐6G_C (VM5a) model

By W. Richard Peltier, D. Argus, R. Drummond. 2015

1,248 citations recorded by the source corpus.

Subfields: Atmospheric Science, Oceanography

View Paper: https://www.semanticscholar.org/paper/31133d01b8c60204fa6371bad24f14d38295c201

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In Atmospheric Science

1. P. Whitehouse
2. Isabella Velicogna
3. Erik Ivins
4. F. Landerer
5. David Wiese
6. S. Swenson
7. Eric J. M. Rignot
8. Jeremie Mouginot

In Oceanography

1. P. Whitehouse
2. F. Landerer
3. Isabella Velicogna
4. David Wiese
5. John M. Wahr
6. S. Swenson
7. Erik Ivins
8. P. Ditmar

Citations in the corpus

• Deglaciation of the Eurasian ice sheet complex (2017, methodology): “An alternative to these process-based models are EISC reconstructions developed through glacial isostatic adjustment modelling (Peltier, 2004; Lambeck et al., 2010; Peltier et al., 2015).”
• GIA Model Statistics for GRACE Hydrology, Cryosphere, and Ocean Science (2018, methodology): “New models (including the ICE-6G model, Peltier et al., 2015; Purcell et al.,2016; Roy & Peltier, 2017, and the latest version of the Australian National University (ANU) model, Lambeck et al., 2014, 2017) use considerably more data that constrain moraine position and dating during the ice sheet…”
• The Tides They Are A‐Changin': A Comprehensive Review of Past and Future Nonastronomical Changes in Tides, Their Driving Mechanisms, and Future Implications (2020, background): “During the Last Glacial Maximum (26.5–19 kyr BP; henceforth LGM; Clark et al., 2009; Peltier et al., 2015) large parts of the Northern Hemisphere landmasses were covered by extensive ice sheets which lowered global MSL by 120–130 m, which led to the exposure of most continental shelves.”
• Continuity of the Mass Loss of the World's Glaciers and Ice Caps From the GRACE and GRACE Follow‐On Missions (2020, methodology): “We remove the glacial isostatic adjustment (GIA), that is, the viscoelastic response by the solid Earth after the ice removal at the end of the last ice age, using Geruo et al. (2013) GIA model forced with ICE-6G loading history (Peltier et al., 2015).”
• The PMIP4 Last Glacial Maximum experiments: preliminary results and comparison with the PMIP3 simulations (2021, methodology): “…modelling groups to use one of three separate ice-sheet reconstructions: the original PMIP3-CMIP5 ice sheet to facilitate comparison with the earlier simulations, ICE-6G_C (Argus et al., 2014; Peltier et al., 2015) and GLAC-1D (Lev Tarasov, personal communication, 2016; Ivanovic et al., 2016).”
• Continuity of Ice Sheet Mass Loss in Greenland and Antarctica From the GRACE and GRACE Follow‐On Missions (2020, methodology): “Outside of Greenland and Antarctica, we therefore use A et al. (2013) with ICE6G ice history (Peltier et al., 2015).”
• A new paradigm for large earthquakes in stable continental plate interiors (2016, result): “The regional pattern is consistent with that expected from GIA [Peltier et al., 2015], with extension (up to 10−8 yr−1) coincident with the uplift areas and shortening (1–3×10−9 yr−1) associated with the subsiding forebulge.”
• Optimizing estimates of annual variations and trends in geocenter motion and J2 from a combination of GRACE data and geophysical models (2016, methodology): “GIA model ICE-6G_VM5a is based on the ICE-6G ice history and the VM5a viscosity profile [Peltier et al., 2015].”