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Precession modulation of the South Pacific westerly wind belt over the past million years

Journal Article · · Proceedings of the National Academy of Sciences of the United States of America
 [1];  [2];  [3];  [1];  [4];  [5];  [6];  [7];  [1];  [8]
  1. Alfred-Wegener-Inst. Helmholtz-Zentrum für Polar- und Meeresforschung, Bremerhaven (Germany)
  2. Univ. of California, Berkeley, CA (United States)
  3. Alfred-Wegener-Inst. Helmholtz-Zentrum für Polar- und Meeresforschung, Bremerhaven (Germany); Univ. of Bremen (Germany)
  4. Leibniz Inst. for Baltic Sea Research, Rostock-Warnemunde (Germany)
  5. Utrecht Univ. (The Netherlands)
  6. Univ. of Bremen (Germany)
  7. Pontifical Catholic Univ. of Chile, Santiago (Chile)
  8. Utrecht Univ., Texel (The Netherlands); Vrije Univ., Amsterdam (The Netherlands)
+ Show Author Affiliations
The southern westerly wind belt (SWW) interacts with the Antarctic Circumpolar Current and strongly impacts the Southern Ocean carbon budget, and Antarctic ice-sheet dynamics across glacial–interglacial cycles. We investigated precipitation-driven sediment input changes to the Southeast Pacific off the southern margin of the Atacama Desert over the past one million years, revealing strong precession (19/23-ka) cycles. Our simulations with 2 ocean–atmosphere general circulation models suggest that observed cyclic rainfall changes are linked to meridional shifts in water vapor transport from the tropical Pacific toward the southern Atacama Desert. These changes reflect a precessional modulation of the split in the austral winter South Pacific jet stream. For precession maxima, we infer significantly enhanced rainfall in the southern Atacama Desert due to a stronger South Pacific split jet with enhanced subtropical/subpolar jets, and a weaker midlatitude jet. Conversely, we derive dry conditions in northern Chile related to reduced subtropical/subpolar jets and an enhanced midlatitude jet for precession minima. The presence of precessional cycles in the Pacific SWW, and lack thereof in other basins, indicate that orbital-scale changes of the SWW were not zonally homogeneous across the Southern Hemisphere, in contrast to the hemispherewide shifts of the SWW suggested for glacial terminations. Finally, the strengthening of the jet is unique to the South Pacific realm and might have affected winter-controlled changes in the mixed layer depth, the formation of intermediate water, and the buildup of sea-ice around Antarctica, with implications for the global overturning circulation and the oceanic storage of atmospheric CO2.
Research Organization:
Lawrence Berkeley National Laboratory (LBNL), Berkeley, CA (United States)
Sponsoring Organization:
National Science Foundation (NSF); USDOE Office of Science (SC)
Grant/Contract Number:
AC02-05CH11231
OSTI ID:
1591825
Journal Information:
Proceedings of the National Academy of Sciences of the United States of America, Journal Name: Proceedings of the National Academy of Sciences of the United States of America Journal Issue: 47 Vol. 116; ISSN 0027-8424
Publisher:
National Academy of SciencesCopyright Statement
Country of Publication:
United States
Language:
English

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Cited By (4)

Fe/Ca ratios of splice sediment cores GeoB3375-1 and GeoB15016 dataset January 2019
Benthic oxygen isotope record of splice sediment cores GeoB3375-1 and GeoB15016 dataset January 2019
Grain size distribution of splice sediment cores GeoB3375-1 and GeoB15016 dataset January 2019
Data from: Precession modulation of the South Pacific westerly wind belt over the past million years dataset January 2019

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Related Subjects

54 ENVIRONMENTAL SCIENCES
orbital cycles
paleoclimate
quaternary
southern westerly wind belt