Can increased poleward oceanic heat flux explain the warm Cretaceous climate?
- 1 October 1996
- journal article
- Published by American Geophysical Union (AGU) in Paleoceanography and Paleoclimatology
- Vol. 11 (5), 579-593
- https://doi.org/10.1029/96pa01851
Abstract
No abstract availableKeywords
This publication has 32 references indexed in Scilit:
- A “simulation” of Mid‐Cretaceous climatePaleoceanography and Paleoclimatology, 1995
- Atmospheric Carbon Dioxide Levels Over Phanerozoic TimeScience, 1990
- Mid‐Cretaceous ocean circulation: Results from model sensitivity studiesPaleoceanography and Paleoclimatology, 1990
- A coupled ocean-atmosphere climate model: temperature versus salinity effects on the thermohaline circulationClimate Dynamics, 1989
- Model Simulation of the Cretaceous Ocean CirculationScience, 1989
- Estimating the Meridional Energy Transports in the Atmosphere and OceanJournal of Physical Oceanography, 1985
- A warm, equable Cretaceous: The nature of the problemEarth-Science Reviews, 1983
- Warm saline bottom water in the ancient oceanNature, 1982
- Atmospheric circulation during warm geologic periods: Is the equator-to-pole surface-temperature gradient the controlling factor?Geology, 1982
- Heat Transport by Currents Across 25°N Latitude in the Atlantic OceanScience, 1980