Coupled ocean‐atmosphere model response to freshwater input: Comparison to Younger Dryas Event
- 1 April 1997
- journal article
- Published by American Geophysical Union (AGU) in Paleoceanography and Paleoclimatology
- Vol. 12 (2) , 321-336
- https://doi.org/10.1029/96pa03932
Abstract
No abstract availableKeywords
This publication has 54 references indexed in Scilit:
- Deglacial sea-level record from Tahiti corals and the timing of global meltwater dischargeNature, 1996
- Synchronous changes in atmospheric CH4 and Greenland climate between 40 and 8 kyr BPNature, 1993
- Evidence for massive discharges of icebergs into the North Atlantic ocean during the last glacial periodNature, 1992
- An early Aranuian glacial advance at Cropp River, central Westland, New ZealandJournal of the Royal Society of New Zealand, 1989
- The chronology of the last Deglaciation: Implications to the cause of the Younger Dryas EventPaleoceanography and Paleoclimatology, 1988
- North Atlantic thermohaline circulation during the past 20,000 years linked to high-latitude surface temperatureNature, 1987
- Does the ocean–atmosphere system have more than one stable mode of operation?Nature, 1985
- A water mass model of the World OceanJournal of Geophysical Research: Oceans, 1979
- CLIMATE AND THE OCEAN CIRCULATIONMonthly Weather Review, 1969
- A numerical investigation of the oceanic general circulationTellus, 1967