Physical mechanisms behind biogeochemical glacial‐interglacial CO2 variations
- 15 June 2001
- journal article
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 28 (12), 2421-2424
- https://doi.org/10.1029/2000gl012571
Abstract
No abstract availableThis publication has 32 references indexed in Scilit:
- Thermal acclimation of leaf respiration but not photosynthesis in Populus deltoides×nigraNew Phytologist, 2008
- A sea ice climate switch mechanism for the 100‐kyr glacial cyclesJournal of Geophysical Research: Oceans, 2001
- Sea ice as the glacial cycles’ Climate switch: role of seasonal and orbital forcingPaleoceanography and Paleoclimatology, 2000
- No glacial‐interglacial cycle in the ice volume simulated under a constant astronomical forcing and a variable CO2Geophysical Research Letters, 2000
- The sequence of events surrounding Termination II and their implications for the cause of glacial‐interglacial CO2 changesPaleoceanography and Paleoclimatology, 1998
- Hydrographic changes of the Southern Ocean (southeast Indian Sector) Over the last 230 kyrPaleoceanography and Paleoclimatology, 1996
- C02 and glacial cyclesNature, 1994
- Geochemical cycles in an ocean general circulation model. Preindustrial tracer distributionsGlobal Biogeochemical Cycles, 1993
- Isotopic composition of atmospheric O2 in ice linked with deglaciation and global primary productivityNature, 1985
- Free Oscillations in a Climate Model with Ice-Sheet DynamicsJournal of the Atmospheric Sciences, 1979