Millennial and orbital variations of El Niño/Southern Oscillation and high-latitude climate in the last glacial period

Chris S. M. Turney (), A. Peter Kershaw, Steven C. Clemens, Nick Branch, Patrick T. Moss and L. Keith Fifield
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Chris S. M. Turney: Queen's University
A. Peter Kershaw: Monash University
Steven C. Clemens: Brown University
Nick Branch: University of London
Patrick T. Moss: University of Wisconsin-Madison
L. Keith Fifield: Research School of Physical Sciences and Engineering, Australian National University

Nature, 2004, vol. 428, issue 6980, 306-310

Abstract: Abstract The El Niño/Southern Oscillation (ENSO) phenomenon is believed to have operated continuously over the last glacial–interglacial cycle1. ENSO variability has been suggested to be linked to millennial-scale oscillations in North Atlantic climate during that time2,3, but the proposals disagree on whether increased frequency of El Niño events, the warm phase of ENSO, was linked to North Atlantic warm or cold periods. Here we present a high-resolution record of surface moisture, based on the degree of peat humification and the ratio of sedges to grass, from northern Queensland, Australia, covering the past 45,000 yr. We observe millennial-scale dry periods, indicating periods of frequent El Niño events (summer precipitation declines in El Niño years in northeastern Australia). We find that these dry periods are correlated to the Dansgaard–Oeschger events—millennial-scale warm events in the North Atlantic climate record—although no direct atmospheric connection from the North Atlantic to our site can be invoked. Additionally, we find climatic cycles at a semiprecessional timescale (∼11,900 yr). We suggest that climate variations in the tropical Pacific Ocean on millennial as well as orbital timescales, which determined precipitation in northeastern Australia, also exerted an influence on North Atlantic climate through atmospheric and oceanic teleconnections.

Date: 2004
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DOI: 10.1038/nature02386

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