A coupled climate–ice sheet modeling approach to the Early Cenozoic history of the Antarctic ice sheet
By Robert M. DeConto, David D. Pollard. 2003
184 citations recorded by the source corpus.
Subfields: Atmospheric Science, Global and Planetary Change
View Paper: https://www.semanticscholar.org/paper/885a9cabb08f692bc07aac33dc665d8c2c7d9470
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In Atmospheric Science
In Global and Planetary Change
Citations in the corpus
- Cenozoic sea-level and cryospheric evolution from deep-sea geochemical and continental margin records (2020, background): “GMSL higher than 12 m above modern requires loss of ice sheets in Greenland, West Antarctica, and sensitive areas of East Antarctica, the Wilkes, and Aurora Basins (70).”
- Hysteresis in Cenozoic Antarctic ice-sheet variations (2005, methodology): “First, a suite of five GCM climate simulations is performed, with orbital configurations updated every 10,000 years in order to resolve an idealized orbital cycle with 20, 40 and 80 ka periodicities (explained in detail in DeConto and Pollard, 2003a,b).”