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Climate of the Past An interactive open-access journal of the European Geosciences Union
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Preprints
https://doi.org/10.5194/cp-2018-110
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/cp-2018-110
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

  31 Aug 2018

31 Aug 2018

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This discussion paper is a preprint. It has been under review for the journal Climate of the Past (CP). The manuscript was not accepted for further review after discussion.

High resolution EPICA ice core dust fluxes: intermittency, extremes and Holocene stability

Shaun Lovejoy1 and Fabrice Lambert2 Shaun Lovejoy and Fabrice Lambert
  • 1Physics Department, McGill University, 3600 University st., Montreal, Que. H3A 2T8, Canada
  • 2Department of Physical Geography, Pontificia Universidad Catolica de Chile, Vicuna Mackenna 4860, Santiago, Chile

Abstract. Recent research in climate variability as a function of temporal or spatial scale has shown that the majority of the variance power lies in what has up until now been considered an unimportant background with relatively little power in well-known frequencies, such as daily, seasonal, or orbital oscillations. Atmospheric variability as a function of scale can be divided in various dynamical "regimes" with alternating increasing and decreasing fluctuations: weather, macroweather, climate, macroclimate, megaclimate. Although a vast amount of data is available at small scales, the larger picture is not well constrained due to the scarcity and low resolution of long paleoclimatic time-series. Here, we analyse a unique centimetric resolution dust flux series from the EPICA Dome C ice-core in Antarctica that spans the past 800 000 years. The temporal resolution is 5 years over the last 400 kyrs, and 25 years over the last 800 kyrs, enabling the detailed statistical analysis and comparison of eight glaciation cycles. The main spectral peak of the complete record is superposed on a scaling (power law) process and accounts for only 4–15 % of the variability, the rest being in the scaling continuum, thus inverting the classical notions of foreground and background processes.

We analyzed the glacial-interglacial cycles using two definitions: a fixed duration of 100 kyrs (segments) and a variable duration defined by the interglacial dust minima (cycles). Segments and cycles were further divided into eight consecutive "phases". We found that the first two phases of each segment or cycle showed particularly large macroweather to climate transition scale Tc (around 2 kyrs), whereas later phases feature centennial transition scales (average of 250 kyr). This suggests that interglacials and glacial maxima are exceptionally stable when compared with the rest of a glacial cycle. The Holocene (with Tc ≈ 4 kyrs) had a particularly large Tc but it was not an outlier when compared with the phase 1 and 2 of other cycles. For each phase we quantified the drift, intermittency, and extremeness of the variability. Phases close to the interglacials (1, 2, 8) show low drift, moderate interm–7 display strong drift, weak intermittency, and weaker extremes.

Shaun Lovejoy and Fabrice Lambert

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Shaun Lovejoy and Fabrice Lambert

Shaun Lovejoy and Fabrice Lambert

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Short summary
The Holocene has been strikingly long and stable when compared to earlier interglacials, and some have argued that the Holocene's exceptional stability permitted the development of agriculture and the spread of civilization. We characterize the past 800 000 years using a high resolution dust record from an Antarctic ice core. We find that although the Holocene is particularly stable when compared to other interglacials, it is not an outlier and other factors may have kickstarted civilization.
The Holocene has been strikingly long and stable when compared to earlier interglacials, and...
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