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

@article{Turney2004MillennialAO,
  title={Millennial and orbital variations of El Ni{\~n}o/Southern Oscillation and high-latitude climate in the last glacial period},
  author={Chris S. M. Turney and A. Peter Kershaw and Steven C. Clemens and Nicholas P Branch and Patrick Moss and L. Keith Fifield},
  journal={Nature},
  year={2004},
  volume={428},
  pages={306-310}
}
The El Niño/Southern Oscillation (ENSO) phenomenon is believed to have operated continuously over the last glacial–interglacial cycle. ENSO variability has been suggested to be linked to millennial-scale oscillations in North Atlantic climate during that time, 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… 
Persistent millennial-scale climate variability in the eastern tropical North Pacific over the last two glacial cycles
High-resolution sediment records from the eastern tropical North Pacific (ETNP) spanning the last ~240 ka B.P. were studied to document the nature of millennial-scale climatic events in the tropical
Mechanisms for millennial‐scale global synchronization during the last glacial period
Global climate during the last glacial period was punctuated by abrupt warmings and occasional pulses of freshwater into the North Atlantic that disrupted deepwater production. These massive
Southern Hemisphere climate variability forced by Northern Hemisphere ice-sheet topography
TLDR
A high-resolution water isotope record from West Antarctica is used to demonstrate that interannual to decadal climate variability at high southern latitudes was almost twice as large at the Last Glacial Maximum as during the ensuing Holocene epoch.
ITCZ rather than ENSO signature for abrupt climate changes across the tropical Pacific?
Extratropical Influences on the El Niño–Southern Oscillation through the Late Quaternary
  • A. Bush
  • Environmental Science, Geography
  • 2007
Abstract A sequence of numerical simulations with a coupled atmosphere–ocean general circulation model configured for particular times during the late Quaternary shows that simulated El Nino–Southern
Rapid global ocean-atmosphere response to Southern Ocean freshening during the last glacial
TLDR
It is shown that Southern Ocean freshwater hosing can trigger global change through climate modelling and the alignment of terrestrial, ice and marine 14C and 10Be records, and that Antarctic-sourced salinity anomalies can generate climate changes that are propagated globally via an atmospheric Rossby wave train.
Does the El Niño–Southern Oscillation control the interhemispheric radiocarbon offset?
Abrupt North Atlantic circulation changes in response to gradual CO2 forcing in a glacial climate state
Glacial climate is marked by abrupt, millennial-scale climate changes known as Dansgaard–Oeschger cycles. The most pronounced stadial coolings, Heinrich events, are associated with massive iceberg
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