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1,500-year Cycle in the Arctic Oscillation Identified in Holocene Arctic Sea-ice Drift
Nature Geoscience
  • Dennis Darby, Old Dominion University
  • Joseph D Ortiz, Kent State University - Kent Campus
  • Chester E Grosch
  • Steven P Lund
Publication Date
Document Type
  • palaeoclimate and palaeoceanography,
  • cryospheric science,
  • atmospheric science,
  • oceanography
Weather and climate in the Northern Hemisphere is profoundly affected by the Arctic Oscillation, a quasi-periodic fluctuation in atmospheric pressure that occurs on interannual to interdecadal timescales. Reconstructions of the Arctic Oscillation over longer timescales have suggested additional centennial- to millennial-scale variations in the phase of the oscillation, but often with conflicting results. Here we assess patterns of sea-ice drift in the Arctic Ocean over the past 8,000 years by geochemically determining the source of ice-rafted iron grains in a sediment core off the coast of Alaska. We identify pulses of sediment carried by sea ice from the Kara Sea, which can reach the coast of Alaska only during a strongly positive Arctic Oscillation. On the basis of these observations, we construct a record of the Arctic Oscillation phase, and identify a 1,500-year periodicity similar to that found in Holocene records of ice-rafted debrisin the North Atlantic, distinct from a 1,000-year cycle that has been found in total solar irradiance. We conclude that the 1,500-year cycle in the Arctic Oscillation arises from either internal variability of the climate system or as an indirect response to low-latitude solar forcing.
Citation Information
Dennis Darby, Joseph D Ortiz, Chester E Grosch and Steven P Lund. "1,500-year Cycle in the Arctic Oscillation Identified in Holocene Arctic Sea-ice Drift" Nature Geoscience Vol. 5 (2012) p. 897 - 900
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