Glacial cycles: Toward a new paradigm

By Didier Paillard. 2001

226 citations recorded by the source corpus.

Subfields: Anthropology, Atmospheric Science

View Paper: https://www.semanticscholar.org/paper/832c7ed25b5cf6f74eb2389fc0b76fdd9409978f

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Citations in the corpus

Forecasting: theory and practice (2020, methodology): “We formulated a 3-equation simultaneous model of atmospheric CO2 and Antarctic Temperature and Ice volume over 800,000 years of Ice Ages in 1000-year frequency (Paillard, 2001; Kaufmann and Juselius, 2013).”
The Antarctic ice sheet and the triggering of deglaciations (2004, background): “A definition of distinct climatic states bglacialQ and binterglacialQ are quite natural from records of deep ocean temperature, CO2, or Southern Ocean temperature [5–8], suggesting a link between the rapid disintegration of Northern Hemisphere ice sheets, the high atmospheric CO2 levels during this ”
Simulation of the last glacial cycle with a coupled climate ice-sheet model of intermediate complexity (2009, unknown): “…Ganopolski (2005) has shown that the glacial inception represents a bifurcation transition in the climate-cryosphere system and that the climate system possesses multiple equilibria within the range of Milankovitch forcing, thus supporting the nonlinear paradigm proposed by Paillard (1998, 2001).”
Solar Irradiance Variability and Climate (2013, background): “The various parameters of the Earth’s orbital and rotational motion vary at periods of 23 kyr (precession), 41 kyr (obliquity) and 100 kyr (eccentricity) (e.g., Crucifix, Loutre & Berger 2006; Paillard 2001).”
The importance of precessional signals in the tropical climate (2004, background): “1999), and there is an active debate as to the role of obliquity in late Quaternary climate change (Paillard 2001; Raymo and Nisancioglu 2003).”
Orbital forcing and role of the latitudinal insolation/temperature gradient (2009, methodology): “A simple model incorporating the idea of a non-linear internally driven response has successfully reproduced the pattern of 100 ka cycles over the last 0.8 million years (Paillard 1998, 2001; Parrenin and Paillard 2003).”
The role of orbital forcing, carbon dioxide and regolith in 100 kyr glacial cycles (2011, background): “One of the major challenges to the classical Milankovitch theory is the presence of 100 kyr cycles that dominate global ice volume and climate variability over the past million years (Hays et al., 1976; Imbrie et al., 1993; Paillard, 2001).”