中国物理B ›› 2014, Vol. 23 ›› Issue (4): 40202-040202.doi: 10.1088/1674-1056/23/4/040202

• GENERAL • 上一篇    下一篇

A class of asymptotic solution for the time delay wind field model of an ocean

周先春a b c, 石兰芳d, 莫嘉琪e   

  1. a College of Electronic and Information Engineering, Nanjing University of Information Science and Technology (NUIST), Nanjing 210044, China;
    b Jiangsu Technology and Engineering Center for Meteorological Sensor Network, Nanjing University of Information Scienceand Technology (NUIST), Nanjing 210044, China;
    c Jiangsu Key Laboratory of Meteorological Observation and Information Processing, Nanjing University of Information Scienceand Technology (NUIST), Nanjing 210044, China;
    d College of Mathematics and Statistics, Nanjing University of Information Science and Technology (NUIST), Nanjing 210044, China;
    e Department of Mathematics, Anhui Normal University, Wuhu 241003, China
  • 收稿日期:2013-06-21 修回日期:2013-09-20 出版日期:2014-04-15 发布日期:2014-04-15
  • 基金资助:
    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), and the Advance Research Foundation in NUIST of China (Grant Nos. 20110371 and 20110385).

A class of asymptotic solution for the time delay wind field model of an ocean

Zhou Xian-Chun (周先春)a b c, Shi Lan-Fang (石兰芳)d, Mo Jia-Qi (莫嘉琪)e   

  1. a College of Electronic and Information Engineering, Nanjing University of Information Science and Technology (NUIST), Nanjing 210044, China;
    b Jiangsu Technology and Engineering Center for Meteorological Sensor Network, Nanjing University of Information Scienceand Technology (NUIST), Nanjing 210044, China;
    c Jiangsu Key Laboratory of Meteorological Observation and Information Processing, Nanjing University of Information Scienceand Technology (NUIST), Nanjing 210044, China;
    d College of Mathematics and Statistics, Nanjing University of Information Science and Technology (NUIST), Nanjing 210044, China;
    e Department of Mathematics, Anhui Normal University, Wuhu 241003, China
  • Received:2013-06-21 Revised:2013-09-20 Online:2014-04-15 Published:2014-04-15
  • Contact: Zhou Xian-Chun E-mail:zhouxc2008@163.com
  • About author:02.30.Mv
  • Supported by:
    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), and the Advance Research Foundation in NUIST of China (Grant Nos. 20110371 and 20110385).

PDF (PC)

339

赞

摘要： A time delay model of a two-layer barotropic ocean with Rayleigh dissipation is built. Using the improved perturbation 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.

关键词: two-layers barotropic, time delay model, asymptotic method

Abstract: A time delay model of a two-layer barotropic ocean with Rayleigh dissipation is built. Using the improved perturbation 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.

Key words: two-layers barotropic, time delay model, asymptotic method

中图分类号:  (Approximations and expansions)

  • 02.30.Mv