CLASSICAL AREAS OF PHENOMENOLOGY |
Prev
Next
|
|
|
Study of scattering from time-varying Gerstners sea surface using second-order small slope approximation |
Zhang Yan-Min(张彦敏)a), Wang Yun-Hua(王运华)b)†, and Guo Li-Xin(郭立新)c) |
a Department of Physics, Ocean University of China, Qingdao 266100, China; b Ocean Remote Sensing Key Laboratory of Ministry of Education, Ocean University of China, Qingdao 266003, China; c School of Science, Xidian University, Xi'an 710071, China |
|
|
Abstract Backscattered fields from one-dimensional time-varying Gerstners sea surface are calculated utilising the second-order small slope approximation. It is well known that spectral properties of the backscattered echoes relate to the velocity of the small elementary scatterers on sea surface profiles. Therefore, modeling Doppler spectra from the ocean requires an accurate description of the sea surface motion. The profile of nonlinear Gerstners sea surface shows vertical-skewness of sea waves, it is sharper at the crest and flatter at the trough than linear waves, and its maximum slope position is closer to the crest than to the trough. Furthermore, the horizontal component of the small elementary scatterers orbit velocity on the sea surface, which yields noticeable influence on Doppler spectra, can be obtained conveniently by Gerstners sea surface model. In this study, the characteristics of Doppler spectra of backscattered fields from time-varying Gerstners sea surface are investigated and the dependences of the Doppler frequency and the Doppler bandwidth on the parameters, such as the wind speed, the radar frequency, the incident angle, etc. are discussed. It is shown that the Doppler bandwidth of microwave scattered fields from Gerstners sea surface is considerably broadened. For the case of high frequency backscattered fields, the values of the higher-order spectrum peaks are larger than those obtained by linear sea surface.
|
Received: 12 September 2009
Revised: 20 October 2009
Accepted manuscript online:
|
PACS:
|
92.60.Ta
|
(Electromagnetic wave propagation)
|
|
92.10.Fj
|
(Upper ocean and mixed layer processes)
|
|
92.10.Hm
|
(Ocean waves and oscillations)
|
|
92.60.Gn
|
(Winds and their effects)
|
|
Fund: Project supported by the Young
Scientists Fund of the National Natural Science Foundation of China
(Grant No.~40906088), the National Natural Science Foundation of
China (Grant No.~60971067) and Specialised Research Fund for the
Doctoral Program of Higher Education (Grant No.~200804231021). |
Cite this article:
Zhang Yan-Min(张彦敏), Wang Yun-Hua(王运华), and Guo Li-Xin(郭立新) Study of scattering from time-varying Gerstners sea surface using second-order small slope approximation 2010 Chin. Phys. B 19 054103
|
[1] |
Toporkov J V and Brown G S 2000 IEEE Trans. Geosci. Remote Sensing 38 1616
|
[2] |
Apel J R 1994 J. Geophys. Res. 99 16269
|
[3] |
Rino C L, Crystal T L, Koide A K, Ngo H D and Guthart H 1991 Radio Sci. 26 51
|
[4] |
Johnson J T, Toporkov J V and Brown G S 2001 IEEE Trans. Geosci. Remote Sensing 39 2411
|
[5] |
Guo L X, Wang R, Wang Y H and Wu Z S 2008 Acta Phys. Sin. 57 3464 (in Chinese)
|
[6] |
Guo L X, Wang R, Wang Y H and Wu Z S 2005 Acta Phys. Sin. 54 96 (in Chinese)
|
[7] |
Barrick D E 1977 Remote Sensing Environ. 6 201
|
[8] |
Barrick D E 1977 Radio Sci. 12 415
|
[9] |
Lipa B 1978 J. Geophys. Res. 83 959
|
[10] |
Gerstner F J 1809 Also Reprinted in Ann. der Physik 32 412
|
[11] |
Rankine W J 1863 Phil. Trans. R. Soc. A 153 127
|
[12] |
Voronovich A G and Zavorotny V U 2001 Waves in Random Media 11 247
|
[13] |
Wen S C 1962 Theory of Ocean Waves (Ji'nan: Shandong Peoples Publishing House) (in Chinese)
|
[14] |
Toporkov J V, Awadallah R S and Brown G S 1999 J. Opt. Soc. Am. A 16 176
|
[15] |
Longuet-Higgins M S 1975 J. Geophys. Res. 80 2688
|
[16] |
Keller M S, Plant W J, Petitt R A and Terray E A 1994 J. Geophys. Res. 99 9751
|
[17] |
Bass F G, Fuks I M, Kalmykov A I, Ostrovsky I E and Rosenberg A D 1968 IEEE Trans. Antennas Propagat. 16 554
|
[18] |
Derr V E 1972 Remote Sensing of the Troposphere (Washington, D.C: U.S.Govt. Printing Office) Chap.12
|
[19] |
Lee P H Y, Barter J D, Beach K L, Lake B M, Rungaldier H, Thompson H R, Wang L and Yee R 1999 Radio Sci. 34 123
|
[20] |
Romeiser R and Thompson D R 2000 IEEE Trans. Geosci. Remote Sensing 38 446
|
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
|
|
|