摘要
将描写海温和气温交互作用的随机动力模式化为一个Fokker-Planck方程(FPE),然后用矩阵连分法进行求解,并对二氧化碳增温效应进行了计算。当CO2从330ppm增加到660ppm时增温1.2℃,模式中存在的优势周期为3~4年,当CO2倍增时各周期有延长的趋势。
The stochastic dynamic model describing the air sea interaction is transformed into a Fokker Planck equation that is then solved by the matrix continuous fraction method. As an example of the solution, the warming by CO 2 increase is calculated and its increment is 1.2 ℃ while CO 2 concentration in the atmosphere increases from 330 to 660 ppm. In the model the dominant period is 3~4 years and it is revealed that the periods tend to get longer when CO 2 doubling occurs.
出处
《南京气象学院学报》
CSCD
1997年第3期410-415,共6页
Journal of Nanjing Institute of Meteorology
基金
扬州大学农学院青年基金
关键词
气候模式
海气耦合
F-P方程
随机动力模式
climatic model, air sea interaction, Fokker Planck equation, matrix continuous fraction method