摘要
A time delay model of a two-layer barotropic ocean with Rayleigh dissipation is built. Using the improved perturba- tion method, an analytic asymptotic solution of a better approximate degree is obtained in the mid-latitude wind field, and the physical meaning of the corresponding solution is also discussed.
A time delay model of a two-layer barotropic ocean with Rayleigh dissipation is built. Using the improved perturba- tion method, an analytic asymptotic solution of a better approximate degree is obtained in the mid-latitude wind field, and the physical meaning of the corresponding solution is also discussed.
基金
Project supported by the National Natural Science Foundation of China(Grant Nos.11202106 and 61302188)
the Specialized Research Fund for the Doctoral Program of Higher Education,China(Grant No.20123228120005)
the Fund from the Jiangsu Sensor Network and Modern Meteorological Equipment Preponderant Discipline Platform,China
the Natural Science Fundation from the Universities of Jiangsu Province,China(Grant No.13KJB170016)
the Advance Research Foundation in NUIST of China(Grant Nos.20110371 and 20110385)
