Numerical simulation of scatterometer assimilated wind and ocean wave in eastern China seas and adjacent waters

Li Mingkui; Hou Yijun; Yin Baoshu; Song Jinbao; Zhao Wei

doi:10.1007/BF02842773

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Numerical simulation of scatterometer assimilated wind and ocean wave in eastern China seas and adjacent waters

OriginalPaper | Updated：2023-05-16

- Numerical simulation of scatterometer assimilated wind and ocean wave in eastern China seas and adjacent waters
- Numerical simulation of scatterometer assimilated wind and ocean wave in eastern China seas and adjacent waters
- 海洋湖沼学报（英文） 2006年24卷第1期页码：42-47
- Affiliations：
  
  Institute of Oceanology Chinese Academy of Sciences
- Author bio：
- Funds：
  
  Supported by the High-Tech Research and Development Program of China (863 Program, No. 2001AA633070;2003AA604040), and the National Natural Science Foundation of China (No. 40476015).
- DOI：10.1007/BF02842773
  中图分类号：
- 纸质出版：2006
- Accepted：
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Numerical simulation of scatterometer assimilated wind and ocean wave in eastern China seas and adjacent waters[J]. 海洋湖沼学报（英文）, 2006,24(1):42-47.

Mingkui, L., Yijun, H., Baoshu, Y. et al. Numerical simulation of scatterometer assimilated wind and ocean wave in eastern China seas and adjacent waters., Chin. J. Ocean. Limnol. 24, 42–47 (2006). https://doi.org/10.1007/BF02842773
Numerical simulation of scatterometer assimilated wind and ocean wave in eastern China seas and adjacent waters[J]. 海洋湖沼学报（英文）, 2006,24(1):42-47. DOI： 10.1007/BF02842773.

Mingkui, L., Yijun, H., Baoshu, Y. et al. Numerical simulation of scatterometer assimilated wind and ocean wave in eastern China seas and adjacent waters., Chin. J. Ocean. Limnol. 24, 42–47 (2006). https://doi.org/10.1007/BF02842773 DOI：

摘要

Abstract

Using the latest version of Mesoscale Modeling System (MM5v3)

we assimilated wind data from the scatterometer and built a model to assimilate the wind field over eastern China seas and adjacent waters and applied the wave model WAVEWATCH-III to test the sea area with assimilative wind and blended wind of QSCAT and NCEP as driving forces. High precision and resolution numerical wave results were obtained. Analysis indicated that if we replace the model wind result with the blended wind

better sea surface wind results and wave results could be obtained.

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Keywords

references

Tolman, H. L., 2002. User Manual and System Documentation of WAVEWATCH-III Version 2.22. Technical Note. US Department of Commerce, National Oceanic and Atmospheric Administration (NOAA)

Dudhia, J., D. Gill, Y. R. Guo and K. Manning, 2000. PSU/NCAR Mesoscale Modeling System Tutorial Class Notes and User's Guide: MM5 Modeling System Version 3.

Lin, M. S., Y. Sun and S. Q. Zheng, 1997. A study on the inversion method of measuring oceanic wind vectors field with the microwave scatterometer carried by satellite.Acta Oceanologica Sinica 19(5): 35–46 (in Chinese)

Lin, M. S., S. Q. Zheng and Y. Sun, 1996. A study on a new dealias algorithm for retrieval of oceanic wind vectors field.Journal of Oceanography In Taiwan Strait 15(3): 243–254. (in Chinese)

Qi, Y. Q., P. C. Chu, P. Shi, Q. W. Mao and C. W. Fan, 2003. Analysis of significant wave heights from WWATCH and TOPEX/Poseidon Altimetry.Acta Oceanologica Sinica 25(4): 1–9. (in Chinese)

Qian, Z. C., 1991. Ocean Waves and Forecasting. Meteorological Publishing Company, Beijing, China. 189p. (in Chinese)

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