|
|
|
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 |
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 |
|
|
|
|
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.
|
Received: 21 June 2013
Revised: 20 September 2013
Accepted manuscript online:
|
|
PACS:
|
02.30.Mv
|
(Approximations and expansions)
|
|
| Fund: 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). |
Corresponding Authors:
Zhou Xian-Chun
E-mail: zhouxc2008@163.com
|
| About author: 02.30.Mv |
Cite this article:
Zhou Xian-Chun (周先春), Shi Lan-Fang (石兰芳), Mo Jia-Qi (莫嘉琪) A class of asymptotic solution for the time delay wind field model of an ocean 2014 Chin. Phys. B 23 040202
|
| [1] |
Zhou T J, Wu B and Wang B 2009 J. Climate 22 1159
|
| [2] |
Zhou T J and Zou L 2010 J. Climate 23 6009
|
| [3] |
Zhou T J and Zhang J 2011 J. Climate 24 1053
|
| [4] |
Cabanes C, Huck T and De Verderce A G 2006 J. Phys. Oceanogyr. 36 1739
|
| [5] |
Qiu B and Chen S M 2006 J. Phys. Oceanogyr. 36 1751
|
| [6] |
Zhang Y C, Lu K C and Zhang M 2011 Sci. Meteorodog. Sin. 31 11 (in Chinese)
|
| [7] |
Lu K C, Zhang Y C and Zhang M 2011 Sci. Meteorodog. Sin. 31 17 (in Chinese)
|
| [8] |
Zhang Y C, Lu K C and Zhang M 2012 Clinmatic and Environmental Research 17 217
|
| [9] |
Zhang H Q and Ding Q 2009 Chin. Phys. Lett. 26 104701
|
| [10] |
Lin W T, Zhang Yu and Mo J Q 2013 Chin. Phys. B 22 030205
|
| [11] |
Mo J Q and Lin W T 2008 Acta Phys. Sin. 57 1291 (in Chinese)
|
| [12] |
Lin Y H, Lin W T and Mo J Q 2009 Acta Phys. Sin. 58 6692 (in Chinese)
|
| [13] |
Mo J Q, Lin Y W and Lin W T 2010 Acta Phys. Sin. 59 6701 (in Chinese)
|
| [14] |
Barbu L and Morosanu G 2007 Singularly Perturbed Boundary-Value Problems (Basel: Birkhauserm Verlag AG)
|
| [15] |
Ramos M 2009 J. Math. Anal. Appl. 352 246
|
| [16] |
D'Aprile T and Pistoia A 2010 J. Diff. Eqs. 248 556
|
| [17] |
Faye L, Frenod E and Seck D 2011 Discrete Contin. Dyn. Sys. 29 1001
|
| [18] |
Shi L F, Lin W T, Lin Y H and Mo J Q 2013 Acta Phys. Sin. 62 010201 (in Chinese)
|
| [19] |
Shi L F and Mo J Q 2013 Acta Phys. Sin. 62 040203 (in Chinese)
|
| [20] |
Mo J Q 2009 Sci. China G 39 568
|
| [21] |
Mo J Q 2011 Acta Phys. Sin. 60 090203 (in Chinese)
|
| [22] |
Mo J Q 2010 Commun. Theor. Phys. 53 440
|
| [23] |
Mo J Q, Lin W T and Lin Y H 2011 Chin. Phys. B 20 070205
|
| No Suggested Reading articles found! |
|
|
Viewed |
|
|
|
Full text
|
|
|
|
|
Abstract
|
|
|
|
|
Cited |
|
|
|
|
Altmetric
|
|
blogs
Facebook pages
Wikipedia page
Google+ users
|
Online attention
Altmetric calculates a score based on the online attention an article receives. Each coloured thread in the circle represents a different type of online attention. The number in the centre is the Altmetric score. Social media and mainstream news media are the main sources that calculate the score. Reference managers such as Mendeley are also tracked but do not contribute to the score. Older articles often score higher because they have had more time to get noticed. To account for this, Altmetric has included the context data for other articles of a similar age.
View more on Altmetrics
|
|
|
