Contrasting scaling properties of interglacial and glacial climates

Type Article
Date 2016-03
Language English
Author(s) Shao Zhi-Gang1, Ditlevsen Peter D.2
Affiliation(s) 1 : S China Normal Univ, SPTE, Guangdong Prov Key Lab Quantum Engn & Quantum Mat, Guangzhou 510006, Guangdong, Peoples R China.
2 : Univ Copenhagen, Niels Bohr Inst, Ctr Ice & Climate, Juliane Maries Vej 30, DK-2100 Copenhagen, Denmark.
Source Nature Communications (2041-1723) (Nature Publishing Group), 2016-03 , Vol. 7 , N. 10951 , P. 8p.
DOI 10.1038/ncomms10951
WOS© Times Cited 27
Abstract

Understanding natural climate variability is essential for assessments of climate change. This is reflected in the scaling properties of climate records. The scaling exponents of the interglacial and the glacial climates are fundamentally different. The Holocene record is monofractal, with a scaling exponent H similar to 0.7. On the contrary, the glacial record is multifractal, with a significantly higher scaling exponent H similar to 1.2, indicating a longer persistence time and stronger nonlinearities in the glacial climate. The glacial climate is dominated by the strong multi-millennial Dansgaard-Oeschger (DO) events influencing the long-time correlation. However, by separately analysing the last glacial maximum lacking DO events, here we find the same scaling for that period as for the full glacial period. The unbroken scaling thus indicates that the DO events are part of the natural variability and not externally triggered. At glacial time scales, there is a scale break to a trivial scaling, contrasting the DO events from the similarly saw-tooth-shaped glacial cycles.

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