A coupled model study of the Last Glacial Maximum: Was part of the North Atlantic relatively warm?
- 15 April 2001
- journal article
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 28 (8), 1571-1574
- https://doi.org/10.1029/2000gl012575
Abstract
No abstract availableThis publication has 22 references indexed in Scilit:
- Reconstruction of sea-surface temperature, salinity, and sea-ice cover in the northern North Atlantic during the last glacial maximum based on dinocyst assemblagesCanadian Journal of Earth Sciences, 2000
- The simulation of SST, sea ice extents and ocean heat transports in a version of the Hadley Centre coupled model without flux adjustmentsClimate Dynamics, 2000
- The Role of Ocean-Atmosphere Interactions in Tropical Cooling During the Last Glacial MaximumScience, 1998
- Simulation of modern and glacial climates with a coupled global model of intermediate complexityNature, 1998
- Climatic Changes of the Last 18,000 Years: Observations and Model SimulationsScience, 1988
- The influence of continental ice, atmospheric CO2, and land albedo on the climate of the last glacial maximumClimate Dynamics, 1987
- Deep Circulation of the North Atlantic over the Last 200,000 Years: Geochemical EvidenceScience, 1982
- Temperature and circulation changes in the eastern North Atlantic during the last 150,000 years: Evidence from the planktonic foraminiferal recordMarine Micropaleontology, 1981
- Modeling the Ice-Age ClimateScience, 1976
- Surface Thermal Boundary Condition for Ocean Circulation ModelsJournal of Physical Oceanography, 1971