Bifurcations and strange nonchaotic attractors in a phase oscillator model of glacial-interglacial cycles

被引:12
作者
Mitsui, Takahito [1 ]
Crucifix, Michel [1 ]
Aihara, Kazuyuki [2 ]
机构
[1] Catholic Univ Louvain, Earth & Life Inst, Georges Lemaitre Ctr Earth & Climate Res, Pl Louis Pasteur 3, BE-1348 Louvain La Neuve, Belgium
[2] Univ Tokyo, Inst Ind Sci, Meguro Ku, Tokyo 1538505, Japan
基金
欧洲研究理事会;
关键词
Glacial-interglacial cycles; Ice age; Quasiperiodically forced dynamical systems; Strange nonchaotic attractor; SNA; Nonsmooth saddle-node bifurcations; Middle-Pleistocene transition; ICE-SHEET MODEL; CLIMATE SYSTEM; INSOLATION; FRACTALIZATION; TORUS; SYNCHRONIZATION; SIMULATION; PACEMAKER; LOCKING; ORIGIN;
D O I
10.1016/j.physd.2015.05.007
中图分类号
O29 [应用数学];
学科分类号
070104 ;
摘要
Glacial-interglacial cycles are large variations in continental ice mass and greenhouse gases, which have dominated climate variability over the Quaternary. The dominant periodicity of the cycles is similar to 40 kyr before the so-called middle Pleistocene transition between similar to 1.2 and similar to 0.7 Myr ago, and it is similar to 100 kyr after the transition. In this paper, the dynamics of glacial-interglacial cycles are investigated using a phase oscillator model forced by the time-varying incoming solar radiation (insolation). We analyze the bifurcations of the system and show that strange nonchaotic attractors appear through nonsmooth saddle-node bifurcations of tori. The bifurcation analysis indicates that mode-locking is likely to occur for the 41 kyr glacial cycles but not likely for the 100 kyr glacial cycles. The sequence of mode-locked 41 kyr cycles is robust to small parameter changes. However, the sequence of 100 kyr glacial cycles can be sensitive to parameter changes when the system has a strange nonchaotic attractor. (C) 2015 Elsevier B.V. All rights reserved.
引用
收藏
页码:25 / 33
页数:9
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