The role of ocean-atmosphere reorganizations in glacial cycles
- 31 October 1989
- journal article
- Published by Elsevier BV in Geochimica et Cosmochimica Acta
- Vol. 53 (10), 2465-2501
- https://doi.org/10.1016/0016-7037(89)90123-3
Abstract
No abstract availableKeywords
This publication has 100 references indexed in Scilit:
- The cause of the glacial to interglacial atmospheric CO2 change: A Polar Alkalinity HypothesisGlobal Biogeochemical Cycles, 1989
- Radiocarbon‐based chronology for the 18O/16O record for the Last DeglaciationPaleoceanography and Paleoclimatology, 1988
- Cadmium: Chemical tracer of deepwater paleoceanographyPaleoceanography and Paleoclimatology, 1988
- Deepwater source variations during the last climatic cycle and their impact on the global deepwater circulationPaleoceanography and Paleoclimatology, 1988
- The chronology of the last Deglaciation: Implications to the cause of the Younger Dryas EventPaleoceanography and Paleoclimatology, 1988
- The influence of continental ice, atmospheric CO2, and land albedo on the climate of the last glacial maximumClimate Dynamics, 1987
- The impact of cold North Atlantic sea surface temperatures on climate: implications for the Younger Dryas cooling (11?10 k)Climate Dynamics, 1986
- Sensitivity Experiments with a Model of the Ice Age Cycle: The Response to Harmonic ForcingJournal of the Atmospheric Sciences, 1985
- The deep waters of the western North Atlantic during the past 24,000 years, and the re-initiation of the Western Boundary UndercurrentMarine Micropaleontology, 1979
- Insolation changes, ice volumes, and the O18 record in deep‐sea coresReviews of Geophysics, 1970