A sea ice climate switch mechanism for the 100‐kyr glacial cycles

By H. Gildor, Eli Tziperman. 2001

146 citations recorded by the source corpus.

Subfields: Atmospheric Science, Environmental Chemistry

View Paper: https://www.semanticscholar.org/paper/ca64bede1ff23f7b4b8bc036a0951ff7bdf1c037

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In Atmospheric Science

In Environmental Chemistry

Citations in the corpus

The physics of climate variability and climate change (2019, background): “The two peaks at about 20 kyr and 40 kyr reflect variations in Earth’s orbit, while the dominant peak at 100 kyr remains to be convincingly explained (Ghil, 1994; Gildor and Tziperman, 2001; Imbrie and Imbrie, 1986).”
Coherent Resonant Millennial-Scale Climate Oscillations Triggered by Massive Meltwater Pulses (2003, background): “…and Sarachik 1991; Sakai and Peltier 1995, 1996, 1997, 1999, 2001; Peltier and Sakai 2001; Bjornsson and Mysak 2001; Winton and Sarachik 1993; Haarsma et al. 2001; Weaver and Hughes 1994; Aeberhardt et al. 2000; Pierce et al. 1996; Winton 1997; Paul and Schulz 2002) that centennial to…”
On the mid-Pleistocene transition to 100-kyr glacial cycles and the asymmetry between glaciation and deglaciation times (2003, background): “…asymmetry which are provided here supplement the predictions based on the sea-ice switch mechanism for the general structure of the land-ice record [Gildor and Tziperman, 2001b], for the role of Milankovitch forcing and the climate transition of 800 kyr ago [Gildor and Tziperman, 2000], for a…”
The role of orbital forcing, carbon dioxide and regolith in 100 kyr glacial cycles (2011, background): “In view of this long-standing problem, it was proposed that the 100 kyr cycles do not originate directly from the orbital forcing but rather represent internal oscillations in the climate-cryosphere (Gildor and Tziperman, 2001) or climate-cryosphere-carbonosphere system (e.”