Quantifying the role of geographic change in Cenozoic ocean heat transport using uncoupled atmosphere and ocean models
- 18 August 2000
- journal article
- Published by Elsevier in Palaeogeography, Palaeoclimatology, Palaeoecology
- Vol. 161 (3-4), 295-310
- https://doi.org/10.1016/s0031-0182(00)00072-9
Abstract
No abstract availableKeywords
This publication has 49 references indexed in Scilit:
- A “simulation” of Mid‐Cretaceous climatePaleoceanography and Paleoclimatology, 1995
- Past climate and the role of ocean heat transport: Model simulations for the CretaceousPaleoceanography and Paleoclimatology, 1993
- Campanian to paleocene spore and pollen assemblages of Seymour Island, AntarcticaReview of Palaeobotany and Palynology, 1990
- Climate variations and the Appalachians from the late paleozoic to the present: Results from model simulationsGeomorphology, 1989
- The hydrologic cycle: A major variable during earth historyPalaeogeography, Palaeoclimatology, Palaeoecology, 1989
- Explanations of the tertiary global cooling trendPalaeogeography, Palaeoclimatology, Palaeoecology, 1985
- Continental distribution as a forcing factor for global-scale temperatureNature, 1984
- The role of geographic variables in explaining paleoclimates: Results from Cretaceous climate model sensitivity studiesJournal of Geophysical Research: Atmospheres, 1984
- Cretaceous climate: A comparison of atmospheric simulations with the geologic recordPalaeogeography, Palaeoclimatology, Palaeoecology, 1982
- Paleogeography as a climatic forcing factorInternational Journal of Earth Sciences, 1981