Sea ice as the glacial cycles' climate switch: Role of seasonal and orbital forcing

By H. Gildor, Eli Tziperman. 2000

194 citations recorded by the source corpus.

Subfields: Atmospheric Science, Environmental Chemistry

View Paper: https://www.semanticscholar.org/paper/217bc37b95b69618fe577f0e0f0ebc6bcf085aab

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

1. L. Lisiecki
2. A. Ridgwell
3. M. Maslin
4. Eli Tziperman
5. H. Gildor
6. M. Raymo
7. Carl Wunsch
8. Linda Hinnov

In Environmental Chemistry

1. L. Lisiecki
2. Eli Tziperman
3. H. Gildor
4. M. Raymo
5. Carl Wunsch
6. A. Ridgwell
7. M. Maslin

Citations in the corpus

• On the mid-Pleistocene transition to 100-kyr glacial cycles and the asymmetry between glaciation and deglaciation times (2003, background): “…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 teleconnection mechanism between the hemispheres, and for the physical processes behind glacial-interglacial CO2…”
• Links between eccentricity forcing and the 100,000-year glacial cycle (2010, background): “2 Myr ago, supporting the hypothesis that 100,000-yr glacial cycles are pace”
• Mid-Pleistocene revolution and the ‘eccentricity myth’ (2005, background): “In one version of this, Gildor & Tziperman (2000) and Tziperman & Gildor (2003) suggest that long term cooling of the deep ocean during the Pleistocene alters the relationship between atmospheric temperature and accumulation rates of snow on continental ice sheets and the growth of sea ice.”
• The 41 kyr world: Milankovitch's other unsolved mystery (2003, background): “Finding an explanation for late Pliocene to early Pleistocene global climate variations represents one of the most interesting and challenging problems facing climate modelers today.”
• Consequences of pacing the Pleistocene 100 kyr ice ages by nonlinear phase locking to Milankovitch forcing (2006, background): “The mechanism of the oscillation is the sea ice switch mechanism of Gildor and Tziperman [2000]. The specifics of the mechanism as well as the fact that it is self-sustained are not relevant, as the”