摘要
假定行星反照率为温度的平方关系,导出了零维随机动力气候模式。对相应的FokkerPlanck方程用矩阵连分法求解,得到了10万年,4万年,2万年气候周期的本征值和本征向量。数值计算表明,在随机噪声强度D=1.95时,10万年气候振动具有最大的振幅,即Milankovitch理论无法解释的10万年周期。
Assuming the planetary albedo is equal to a temperature square. a zero-dimensional stochastic-dynamic climate model has been suggested. The appropriate Fokker-Planck equation is solved by use of the matrix continude-fraction method, eigen values and eigen vectors of 100 000a, 40 000a and 20 000a climatic periods are obtained. It is shown from the numerical computation that the climatic fluctuation of 100 000a has maximum amplitude when taking intensity of random noise D = 1. 95. the fluctuation is not explained with the Milankovitch theory.
出处
《气象学报》
CSCD
北大核心
1996年第6期753-758,共6页
Acta Meteorologica Sinica
基金
国家自然科学基金
扬州大学农学院院青年基金
关键词
零维气候模式
长期振动
F-P方程
全球气候
Zero-dimensional climate model, Fokker-Planck equation, Matrix continued-fraction method.