为了研究南京局地气候动力系统的演变,利用无量纲处理后的南京站1951—2013年逐年云量、气温和降水资料,采用反演建模方法,构建了1951—2013年南京局地气候模型,并对南京局地气候模型的各项系数进行了初步的物理解释。结果发现,南京局地气候模型中云量指数的变化与云量指数、降水指数和降水指数的二次项有关;气温指数的变化与气温指数、云量指数、降水指数和气温指数的二次项有关;降水指数的变化与降水指数、云量指数和降水指数的二次项有关。以每30年的数据反演局地气候模型,发现非线性部分系数呈减小趋势,其中利用1961—1990年和1962—1991年数据的反演结果中,云量和降水变化方程中降水二次项系数都发生了突变。线性部分在气候态附近保持稳定。
The paper aims to study the evolution of Nanjing local climate dynamic system, the cloud cover,temperature and precipitation data with dimensionless treatment in Nanjing during 1951-2013 were used tobuilt Nanjing local climate model by using inverse model method, and a preliminary physical interpretation ofall coefficients of Nanjing local climate model was conducted. The study showed that: the change of cloud coverindex was related with cloud cover index, precipitation index and square of precipitation index; the change oftemperature index was related with temperature index, cloud cover index, precipitation index and square oftemperature index; the change of precipitation index was related with precipitation index, cloud cover indexand square of precipitation index. By studying the evolution of local climate model using each 30-year data, itwas found that the coefficient of the nonlinear part had a decreasing trend, and the models of 1961- 1990 and 1962-1991 showed a mutation in square of precipitation index in cloud cover and precipitation changeequations. In linear part, it kept stable near climate state.