Stochastic resonance in the North Atlantic

Paleoceanography

Volumn 16, Issue 2, 2001, Pages 190-198

  Alley, R B ^a   Anandakrishnan, S ^b   Jung, P ^c  

^a PENNSYLVANIA STATE UNIVERSITY   (United States)

^b UNIVERSITY OF ALABAMA   (United States)

^c OHIO UNIVERSITY   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

CLIMATE CHANGE; PALEOCEANOGRAPHY; PALEOCLIMATE; PERIODICITY; STOCHASTICITY;

(NORTH); ATLANTIC OCEAN;

EID: 0034984961     PISSN: 08838305     EISSN: None     Source Type: Journal    
DOI: 10.1029/2000PA000518     Document Type: Article

References (39)

1. The deglaciation of the northern Hemisphere: A global perspective
2. Changes in continental and sea-salt atmospheric loadings in central Greenland during the most recent deglaciation: Model-based estimates
3. Comparison of deep ice cores
4. Visual-straugraphic dating of the GISP2 ice core: Basis, reproducibility, and applications
5. Abrupt increase in Greenland snow accumulation at the end of the Younger Dryas event
6. Forcing of the cold event of 8,200 years ago by catastrophic drainage of Laurentide lakes
7. Stochastic resonance in climatic change
8. A pervasive millennialscale cycle in North Atlantic Holocene and glacial climates
9. The North Atlantic's 1-2 kyr climate rhythm: Relation to Heinrich events, Dansgaard/Oeschger cycles and the Little Ice Age
10. The chronology of the last deglaciation: Implications to the cause of the Younger Dryas event
11. A salt oscillator in the glacial Atlantic? I, The concept
12. High-latitude salinity effects and interhemispheric thermohaline circulations
13. A role for the tropical Pacific coupled ocean-atmosphere system on Milankovitch and millennial timescales. Part II: Global impacts
14. CH4 and δ18O of O2 records from Antarctic and Greenland ice: A clue for stratigraphic disturbances in the bottom part of the Greenland Ice core project and the Greenland Ice Sheet Project 2 ice cores
15. Comparison of proxy records of climate change and solar forcing
16. Large Arctic temperature change at the glacial-Holocene transition
17. Holocene climatic variations - their pattern and possible cause
18. Observation of α-stable noise induced millennial climate changes from an ice-core record
19. Stochastic resonance
20. Oxygen 18/16 variability in Greenland snow and ice with 10-3- to 105-year time resolution
21. Irregular glacial interstadials recorded in a new Greenland ice core
22. The δ18O record along the Greenland Ice Core Project deep ice core and the problem of possible Eemian climatic instability
23. Validity of the temperature reconstruction from water isotopes in ice cores
24. The 1800-year oceanic tidal cycle: A possible cause of rapid climate change
25. Glacial-Holocene stratigraphy, chronology, and paleoceanographic observations on some North Atlantic sediment drifts
26. Freshwater routing by the Laurentide Ice Sheet during the last deglaciation
27. Major features and forcing of high-latitude northern hemisphere atmospheric circulation using a 110,000-year-long glaciochemical series
28. A 0.5-million-year record of millennial-scale climate variability in the North Atlantic
29. The Greenland ice sheet project 2 depth-age scale: Methods and results
30. Bifurcations of the Atlantic thermohalme circulation in response to changes in the hydrological cycle
31. A simple model of the Atlantic thermohaline circulation: Internal and forced variability with paleoclimatological implications
32. Changes in east Atlantic deepwater circulation over the last 30,000 years: Eight time slice reconstructions
33. Timing of abrupt climate change at the end of the Younger Dryas interval from thermally fractionated gases in polar ice
34. Influence of COf2 emission rates on the stability of the thermohaline circulation
35. The influence of high-latitude surface forcing on the global thermohaline circulation
36. The Holocene/Younger Dryas transition recorded at Summit, Greenland
37. Rapid interglacial climate fluctuations driven by North Atlantic Ocean circulation
38. On sharp spectral lines in the climate record and the millennial peak
39. Paleoclimatic variability inferred from the spectral analysis of Greenland and Antarctic ice-core data