摘要:
|
本文将卫垦遥感资料应用在台风数值预报中,并用变分调整方法对客观分析场进行变分调整,最终形成台风数值预报模式的初始场。台风数值预报模式采用σ坐标系中通量形式原始方程组,垂直方向分为三层,水平方向采用三重嵌套网格方案,细网格随台风中心位置的变化而移动。 |
|
参考文献:
|
[1] 吴辉碇,杨学联,白珊.三维斜压台风模式-I.数值方法.海洋学报,1998,20(4): [2] 大河内芳雄移动式多重格子系(MNG)应用.いた台风预报研究时报,39:7-9号,173~198 [3] 张玉玲,吴辉碇,王晓林数值天气预报科学出版社,472 [4] Arakawa, A., Computational design for long-term numerical integration of the equation of atmospheric motion. J. Com putationalPhys., 1, 119-143. [5] Winninghoff, E J. On the adjustment toward a geostrophic balance in a simple primitive equation model with application tothe problem of initialization and objective analysis, Ph D. Thesis, University of California, Los Angeles, 161. [6] Blumberg A. F. and G. L. Melior: A description ora three-dimensional coastal ocean circulation model, Coastal andEstuarine Science 4, Three-Dimensional Coastal Ocean Models, (Heaps. N. S. Ed.), AGUWashingtonD. C., 1-16. [7] Mesinger. F. and A. Arakawa. Numerical Methods Used in AtmophericModels, 1, GARP Publications Series, 17. 64. |
服务与反馈:
|
【文章下载】【发表评论】【查看评论】【加入收藏】
|
|
|