Alley, Richard B. et al. (2001): Stochastic resonance in the North Atlantic; further insights

Leg/Site/Hole:
ODP 162
ODP 162 980
Identifier:
2006-059966
georefid

Creator:
Alley, Richard B.
Pennsylvanian State University, Department of Geosciences, University Park, PA, United States
author

Anandakrishnan, S.
University of College London, United Kingdom
author

Jung, P.
University of Alabama, United States
author

Clough, A.
Ohio University, United States
author

Identification:
Stochastic resonance in the North Atlantic; further insights
2001
In: Seidov, Dan (editor), Haupt, Bernd J. (editor), Maslin, Mark (editor), The oceans and rapid climate change; past, present, and future
American Geophysical Union, Washington, DC, United States
126
57-68
The large, abrupt, widespread, millennial changes recorded in many paleoclimatic archives pose a major challenge to our understanding of the climate system. Both periodic and stochastic models have been proposed to explain these events. We have argued that Greenland ice-core data are more consistent with a stochastic-resonance hypothesis. Here, we show that the stochastic-resonance hypothesis is consistent with a wider range of previously published data than analyzed before including a North Atlantic marine record and the Byrd Station, Antarctica ice-isotopic record. (mod. journ. abst.)
English
Serial
Coverage:Geographic coordinates:
North:55.2906
West:-120.0100East: -14.4208
South:-79.5900

Quaternary geology; Antarctica; Arctic region; Atlantic Ocean; Byrd Station; Cenozoic; climate change; Dansgaard-Oeschger cycles; Foraminifera; Greenland; Greenland ice sheet; Invertebrata; isotope ratios; isotopes; Leg 162; Marie Byrd Land; marine sediments; microfossils; North Atlantic; Northeast Atlantic; O-18/O-16; Ocean Drilling Program; ODP Site 980; oxygen; paleo-oceanography; paleoclimatology; paleotemperature; Pleistocene; Protista; Quaternary; sediments; stable isotopes; stochastic processes; upper Pleistocene;

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