Orbital pacing of methane hydrate destabilization during the Palaeogene

By A. Ridgwell, Dan Lunt, A. Sluijs. 2011

141 citations recorded by the source corpus.

Subfields: Atmospheric Science, Environmental Chemistry, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/84a32e4d7704aaf3d3ff54a150e9e50accc94ee9

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. Robert M. DeConto
2. Matthew Huber
3. B. Wade
4. Dan Lunt
5. S. Wing
6. David D. Pollard
7. N. Stern
8. A. Barnosky

In Environmental Chemistry

1. Robert M. DeConto
2. Matthew Huber
3. N. Stern
4. J. Blois

In Global and Planetary Change

1. Robert M. DeConto
2. Matthew Huber
3. Dan Lunt
4. B. Wade
5. A. Winguth
6. N. Stern

Citations in the corpus

• Cenozoic carbon cycle imbalances and a variable weathering feedback (2016, unknown): “An increase in the feedback strength may result from greater physical denudation in the late Cenozoic that results in a stronger coupling between weathering fluxes and climate (Maher and Chamberlain, 2014; West, 2012).”
• The DeepMIP contribution to PMIP4 (2017, background): “Warming from the five models in “Eomip” (Lunt et al., 2012) are shown as coloured lines; for each model only the CO2 concentration that best fits the temperature proxy observations is shown. Warming derived from the proxies are shown as filled circles, with error bars representing the range of uncer”