Global glacial isostatic adjustment: palaeogeodetic and space‐geodetic tests of the ICE‐4G (VM2) model
By W. Richard Peltier. 2002
158 citations recorded by the source corpus.
Subfields: Atmospheric Science, Geophysics, Oceanography
View Paper: https://www.semanticscholar.org/paper/f80f2b5e5abc344de8df4cec41ec5ed410e7b455
How researchers see this paper
The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.
In Atmospheric Science
- R. Drummond
- D. Argus
- W. Richard Peltier
- L. Tarasov
- P. Whitehouse
- John M. Wahr
- Isabella Velicogna
- M. Tamisiea
In Geophysics
- L. Tarasov
- D. Argus
- R. Drummond
- W. Richard Peltier
- M. Tamisiea
- John C. Moore
- Aslak Grinsted
- Svetlana Jevrejeva
In Oceanography
- R. Drummond
- D. Argus
- W. Richard Peltier
- L. Tarasov
- P. Whitehouse
- John M. Wahr
- M. Tamisiea
- Isabella Velicogna
Citations in the corpus
- A geophysically constrained large ensemble analysis of the deglacial history of the North American ice-sheet complex (2004, methodology): “They are also critical to recent geophysical arguments for the existence of a Keewatin Dome on the Canadian Shield to the west of Hudson Bay (Peltier, 2002a).”
- Space geodesy constrains ice age terminal deglaciation: The global ICE‐6G_C (VM5a) model (2015, background): “Simple ice sheet coupled climate models have been successful in explaining the origins of this 100 kyr cyclic behavior [Tarasov and Peltier, 1997; Peltier, 2002b], but only if the known covariation of atmospheric carbon dioxide is directly employed in addition to orbital insolation change as an…”