The role of orbital forcing, carbon dioxide and regolith in 100 kyr glacial cycles
A. Ganopolski and R. Calov
Related subject area
Subject: Climate Modelling | Archive: Modelling only | Timescale: MilankovitchGreenland climate simulations show high Eemian surface melt which could explain reduced total air content in ice coresThe response of tropical precipitation to Earth's precession: the role of energy fluxes and vertical stabilityInterhemispheric effect of global geography on Earth's climate response to orbital forcing
Clim. Past, 17, 317–330,2021
Clim. Past, 15, 449–462,2019
Clim. Past, 15, 377–388,2019
Bauer, E. and Ganopolski, A.: Aeolian dust modeling over the past four glacial cycles with CLIMBER-2, Global Planet. Change, 74, 49–60, 2010.
Berger A.: Long-term variations of daily insolation and Quaternary climatic change, J. Atmos. Sci., 35, 2362–2367, 1978.
Berger, A., Loutre, M. F., and Gallee, H.: Sensitivity of the LLN climate model to the astronomical and CO2 forcings over the last 200 ky, Clim. Dynam., 14, 615–629, 1998.
Berger, A., Li, X. S., and Loutre, M. F: Modeling northern hemisphere ice volume over the last 3 million years, Quaternary Sci. Rev., 18, 1–11, 1999.
Berger, A., Melice, J. L., and Loutre M. F.: On the origin of the 100-kyr cycles in the astronomical forcing, Paleoceanography, 20, PA4019, https://doi.org/10.1029/2005PA001173, 2005.