Climate evolution in the Pliocene and Pleistocene from marine‐sediment records and simulations: Internal variability versus orbital forcing
- 20 June 1993
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research: Atmospheres
- Vol. 98 (D6) , 10385-10399
- https://doi.org/10.1029/93jd00200
Abstract
No abstract availableKeywords
This publication has 44 references indexed in Scilit:
- Stability of the Astronomical Frequencies Over the Earth's History for Paleoclimate StudiesScience, 1992
- A model for atmospheric CO 2 over Phanerozoic timeAmerican Journal of Science, 1991
- Calibration of the 14C timescale over the past 30,000 years using mass spectrometric U–Th ages from Barbados coralsNature, 1990
- The influence of continental ice, atmospheric CO2, and land albedo on the climate of the last glacial maximumClimate Dynamics, 1987
- The outer solar system for 200 million yearsThe Astronomical Journal, 1986
- “Slow” physics of large continental ice sheets and underlying bedrock and its relation to the Pleistocene ice agesJournal of Geophysical Research, 1985
- The carbonate-silicate geochemical cycle and its effect on atmospheric carbon dioxide over the past 100 million yearsAmerican Journal of Science, 1983
- A Model Study of the Role of High-Latitude Topography in the Climatic Response to Orbital Insolation AnomaliesJournal of the Atmospheric Sciences, 1982
- Long-Term Variations of Daily Insolation and Quaternary Climatic ChangesJournal of the Atmospheric Sciences, 1978
- A study of the stability of a model continental ice sheet subject to periodic variations in heat inputJournal of Geophysical Research, 1977