Evidence for increased latent heat transport during the Cretaceous (Albian) greenhouse warming
- 1 January 2004
- journal article
- Published by Geological Society of America in Geology
- Vol. 32 (12) , 1049
- https://doi.org/10.1130/g20828.1
Abstract
No abstract availableThis publication has 25 references indexed in Scilit:
- High latitude meteoric δ18O compositions: Paleosol siderite in the Middle Cretaceous Nanushuk Formation, North Slope, AlaskaGSA Bulletin, 2004
- The role of ocean heat transport in climatic changePublished by Elsevier ,2003
- Deep water formation and poleward ocean heat transport in the warm climate extreme of the Cretaceous (80 Ma)Geophysical Research Letters, 1998
- Can increased poleward oceanic heat flux explain the warm Cretaceous climate?Paleoceanography and Paleoclimatology, 1996
- A “simulation” of Mid‐Cretaceous climatePaleoceanography and Paleoclimatology, 1995
- Possible role of oceanic heat transport in Early Eocene climatePaleoceanography and Paleoclimatology, 1995
- Past CO2 Changes and Tropical Sea Surface TemperaturesPaleoceanography and Paleoclimatology, 1991
- Mid‐Cretaceous ocean circulation: Results from model sensitivity studiesPaleoceanography and Paleoclimatology, 1990
- Late Cretaceous terrestrial vegetation: A near-polar temperature curveGeology, 1988
- Paleogeography as a climatic forcing factorInternational Journal of Earth Sciences, 1981