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By using the model developed in Part Ⅰ of the sister papers,simulations of severe storm,winter airflow and snowfallover a mountain,as well as mountain-valley winds and sea breeze are performed.Different functions of the model areverified through the computation and special emphasis is put on some important properties of the meso-(β-γ) systemsfrequently occurring.The simulation results of the cases are agreeable to field observations,conceptual models,and pre-vious numerical studies.It is shown that the model is applicable for the researches and prediction of various localand/or regional weather processes,and capable of describing their macro- and micro-structures,influences oforographic and underlying-surface forcing,and interaction between meso-β and meso-γ scales.In addition,theevolutional characteristics and mechanisms of the modeled processes are also analyzed.
By using the model developed in Part I of the sister papers, simulations of severe storm, winter airflow and snowfallover a mountain, as well as mountain-valley winds and sea breeze are performed. Different functions of the model are verified through the computation and emphasis is put on some important properties of the meso- (β-γ) systemsfrequently occurring. The simulation results of the cases are agreeable to field observations, conceptual models, and pre-vious numerical studies. It is shown that the model is applicable for the researches and prediction of various localand / or regional weather processes, and capable of describing their macro- and micro-structures, influences oforographic and underlying-surface forcing, and interaction between meso-β and meso-γ scales. addition, the evolutional characteristics and mechanisms of the modeled processes are also analyzed.