摘要
利用兰州九洲台黄土剖面磁化率资料分析了古气候变化的混沌特性.结果表明,该地区1.4Ma以来的古气候是具有有限个自由度的复杂系统,吸引子的关联维数为4.3。
The nonlinear characteristics of palaeoclimatic variations of Lanzhou have been studied in this paper by using the chaotic method. The time series is 1 4 Ma, while the time interval is 500 years with 2 801 sample points. The calculated results show the palaeoclmatic evolution in Lanzhou is a complex chaotic system with finite degrees of freedom. The association embedded dimension attractor is 4 3, while the saturation dimension is 12.
出处
《兰州大学学报(自然科学版)》
CAS
CSCD
北大核心
1997年第1期120-123,共4页
Journal of Lanzhou University(Natural Sciences)
基金
国家教委优秀中青年教师基金
重点跟踪调查基金