摘要
本文利用Fraedrich,K.参数化讨论了零维能量平衡模式平衡态特性,在此基础上对全球温度变化的随机模式作了重新认识和改进,并用1881—1981年北半球温度距平序列对改进后的模式作了检验。
In this paper the parameterization used by K. Fraedrich is adopted to discuss the characteristics in the equilibrium state of the zerodimensional model, and thereafter the stochastic model for the global temperature changes is reviewed and revised. And then the revised model is checked with the 1881-1981 northern hemisphere temperature anomaly series.
出处
《南京气象学院学报》
CSCD
1990年第1期99-109,共11页
Journal of Nanjing Institute of Meteorology
