A two-parameter stochastic process for Dansgaard-Oeschger events

被引:6
|
作者
Braun, H. [1 ,2 ]
Ditlevsen, P. [2 ]
Kurths, J. [3 ,5 ]
Mudelsee, M. [4 ,6 ]
机构
[1] Heidelberg Acad Sci & Humanities, D-69120 Heidelberg, Germany
[2] Univ Copenhagen, Ctr Ice & Climate, Niels Bohr Inst, DK-2100 Copenhagen, Denmark
[3] Potsdam Inst Climate Impact Res, D-14412 Potsdam, Germany
[4] Climate Risk Anal, D-30167 Hannover, Germany
[5] Humboldt Univ, Inst Phys, Berlin, Germany
[6] Alfred Wegener Inst Polar & Marine Res, D-2850 Bremerhaven, Germany
来源
PALEOCEANOGRAPHY | 2011年 / 26卷
关键词
ABRUPT CLIMATE-CHANGE; GREENLAND ICE CORES; NORTH-ATLANTIC; CYCLE; RESOLUTION; MODEL; CHRONOLOGY; RECORDS; NOISE;
D O I
10.1029/2011PA002140
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Various climatic processes are thought to evolve as rapid, shift-like events, which points at the presence of nonlinear dynamics. Time series analysis of nonlinear processes, however, is not trivial, for example, because of the difficulty in coming up with a realistic random process as a viable null hypothesis. In this methodology paper we construct a basic two-parameter process of shift-like excursions in an excitable system with a threshold. We demonstrate that this stochastic process, in comparison with a specific one-parameter process, can better reproduce main features of the waiting time histogram of abrupt glacial climate events, the Dansgaard-Oeschger events, as seen in two paleoclimatic proxy records, the North Greenland Ice core Project (NGRIP) ice core and the Sofular stalagmite delta O-18 records. We use the two-parameter process to test some arguments that were proposed in the ongoing discussion of a possible solar role in triggering Dansgaard-Oeschger events. Using our approach, we suggest for future studies to generate time series of random events which can serve as a more plausible null hypothesis for Monte Carlo based statistical tests on the regularity of shift-like processes such as Dansgaard-Oeschger events.
引用
收藏
页数:12
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