Multi-scale wavelet analysis of TOPEX/Poseidon altimeter significant wave height in eastern China seas

Guo Yanyou; Hou Yijun; Li Mingkui

doi:10.1007/BF02842779

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Multi-scale wavelet analysis of TOPEX/Poseidon altimeter significant wave height in eastern China seas

OriginalPaper | Updated：2023-05-16

- Multi-scale wavelet analysis of TOPEX/Poseidon altimeter significant wave height in eastern China seas
- Multi-scale wavelet analysis of TOPEX/Poseidon altimeter significant wave height in eastern China seas
- 海洋湖沼学报（英文） 2006年24卷第1期页码：81-86
- Affiliations：
  
  1. Institute of Oceanology Chinese Academy of Sciences
  2. Graduate School 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/BF02842779
  中图分类号：
- 纸质出版：2006
- Accepted：
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Multi-scale wavelet analysis of TOPEX/Poseidon altimeter significant wave height in eastern China seas[J]. 海洋湖沼学报（英文）, 2006,24(1):81-86.

Yanyou, G., Yijun, H. & Mingkui, L. Multi-scale wavelet analysis of TOPEX/Poseidon altimeter significant wave height in eastern China seas., Chin. J. Ocean. Limnol. 24, 81–86 (2006). https://doi.org/10.1007/BF02842779
Multi-scale wavelet analysis of TOPEX/Poseidon altimeter significant wave height in eastern China seas[J]. 海洋湖沼学报（英文）, 2006,24(1):81-86. DOI： 10.1007/BF02842779.

Yanyou, G., Yijun, H. & Mingkui, L. Multi-scale wavelet analysis of TOPEX/Poseidon altimeter significant wave height in eastern China seas., Chin. J. Ocean. Limnol. 24, 81–86 (2006). https://doi.org/10.1007/BF02842779 DOI：

摘要

Abstract

The multi-scale characteristics of wave significant height (H s) in eastern China seas were revealed by multi-scale wavelet analysis. In order to understand the relation between wave and wind

the TOPEX/Poseidon measurements ofH s and wind speed were analyzed. The result showed thatH s and wind speed change in multi-scale at one-

two-month

half-

one- and two-year cycles. But in a larger time scale

the variations inH s and wind speed are different.H s has a five-year cycle similar to the cycle of ENSO variation

while the wind speed has no such cycle. In the time domain

the correlation betweenH s and ENSO is unclear.

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references

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