Influence of ocean heat transport on the climate of the Last Glacial Maximum
- 1 February 1997
- journal article
- research article
- Published by Springer Nature in Nature
- Vol. 385 (6618), 695-699
- https://doi.org/10.1038/385695a0
Abstract
No abstract availableKeywords
This publication has 39 references indexed in Scilit:
- Temperature depression in the lowland tropics in glacial timesClimatic Change, 1996
- Late Pleistocene Temperature Depression and Vegetation Change in Ecuadorian AmazoniaQuaternary Research, 1990
- Temperature and rainfall estimates for the past 40,000 years in equatorial AfricaNature, 1990
- Components of the ice age circulationJournal of Geophysical Research: Atmospheres, 1987
- The influence of continental ice, atmospheric CO2, and land albedo on the climate of the last glacial maximumClimate Dynamics, 1987
- A Comparison of Climate Model Sensitivity with Data from the Last Glacial MaximumJournal of the Atmospheric Sciences, 1985
- Terrestrial Conditions at the Last Glacial Maximum and CLIMAP Sea-Surface Temperature Estimates: Are They Consistent?Quaternary Research, 1985
- Climate sensitivity: Analysis of feedback mechanismsPublished by Wiley ,1984
- Late Quaternary Ice Age Climates of Tropical Australasia: Interpretations and ReconstructionsQuaternary Research, 1978
- Simulation of the tropical climate of an ice ageJournal of Geophysical Research, 1977