Atlantic Ocean heat piracy and the bipolar climate see-saw during Heinrich and Dansgaard-Oeschger events

Journal of Quaternary Science

Volumn 16, Issue 4, 2001, Pages 321-328

  Seidov, Dan ^a,b   Maslin, Mark ^b  

^a PENNSYLVANIA STATE UNIVERSITY   (United States)

^b UNIVERSITY COLLEGE LONDON   (United Kingdom)

Author keywords

Bipolar climate see saw; Dansgaard Oeschger cycles; Deep water circulation; Heinrich events; Hemispheric heat piracy; Ocean circulation modelling

Indexed keywords

HEINRICH EVENT; LAST GLACIAL; PALEOCEANOGRAPHY; PALEOCLIMATE;

ANTARCTICA; ATLANTIC OCEAN; GREENLAND;

EID: 0035019716     PISSN: 02678179     EISSN: None     Source Type: Journal    
DOI: 10.1002/jqs.595     Document Type: Article

References (51)

1. Asynchrony of Antarctic and Greenland climate change during the last glacial period
2. The great ocean conveyor
3. Paleocean circulation during the last deglaciation: A bipolar seesaw?
4. Was a change in thermohaline circulation responsible for the Little Ice Age?
5. High-latitude salinity effects and interhemispheric thermohaline circulations
6. Parameter sensitivity of primitive equation ocean general circulation models
7. A numerical method for the study of the circulation of the world ocean
8. A water-mass model of the world ocean
9. An idealized model of the world ocean, Part 1: The global-scale water masses
10. Evidence for general instability of past climate from a 250-kyr ice-core-record
11. A model study of the Atlantic thermohaline circulation during the Last Glacial Maximum
12. Interocean exchange of thermocline water
13. Climate variability and the Atlantic Ocean
14. Patterns of ice-rafted detritus in the glacial North-Atlantic (40-55°N)
15. Direct estimates and mechanisms of ocean heat transport
16. An ice shelf mechanism for Heinrich layer production
17. Investigating the sensivity of the atmospheric general circulation Model ECHAM 3 to paleoclimate boundary conditions
18. Two stable equilibria of a coupled ocean-atmosphere model
19. Simulation of abrupt change induced by freshwater input to the North Atlantic Ocean
20. Coupled ocean-atmosphere model response to freshwater input: Comparison to Younger Dryas event
21. Multiple equilibria of the global thermohaline circulation
22. Instability and multiple steady states in a meridional-plane model of the thermohaline circulation
23. Surface water temperature, salinity, and density changes in the northest Atlantic during the last 45,000 years: Heinrich events, deep water formation, and climatic rebounds
24. Modeling teleconnections between the North Atlantic and North Pacific during the Younger Dryas
25. Late glacial climate history from ice cores
26. Bifurcations of the Atlantic thermohaline circulation in response to changes in the hydrological cycle
27. Magnetic susceptibility variations in Late Pleistocene deep-sea sediments of the North East Atlantic: Implications for ice rafting and palaeocirculation at the Last Glacial Maximum
28. On the north and tropical Atlantic heat balance
29. Variations in Atlantic Ocean paleoceanography, 50°-85°N: A time-slice record of the last 30,000 years
30. On the interbasin-scale thermohaline circulation
31. On the North Atlantic circulation
32. Simulated ocean circulation and sediment transport in the North Atlantic during the Last Glacial maximum and today
33. Seasonally ice free glacial Nordic Seas without deep water ventilation
34. North Atlantic deep water circulation collapse during the Heinrich events
35. North Atlantic ocean circulation during the Last Glacial Maximum and subsequent meltwater event: A numerical model
36. Synchronous climate changes in Antarctica and the North Atlantic
37. 2 variations
38. The variable ocean
39. The see-saw effect
40. The influence of high-latitude surface forcing on the global thermohaline circulation
41. Effect of Drake Passage on the global thermohaline circulation
42. Simulation of radiocarbon in a coarse-resolution world ocean circulation model, 1. Steady state prebomb distribution
43. Rapid interglacial climate fluctuations driven by North Atlantic ocean circulation
44. Simulated influence of carbon dioxide, orbital forcing and ice-sheets on the climate of the last glacial maximum
45. Influence of ocean heat transport on the climate of the Last Glacial Maximum
46. A zonally averaged ocean model for the thermohaline circulation, I. Model development and flow dynamics