A new model to estimate significant wave heights with ERS- 1/2 scatterometer data
A new model is proposed to estimate the significant wave heights with ERS-1/2 scatterometer data. The results show that the relationship between wave parameters and radar backscattering cross section is similar to that between wind and the radar backscattering cross section. Therefore, the relations...
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          | Published in | Chinese journal of oceanology and limnology Vol. 27; no. 1; pp. 112 - 116 | 
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| Main Author | |
| Format | Journal Article | 
| Language | English | 
| Published | 
        Heidelberg
          SP Science Press
    
        01.02.2009
     Springer Nature B.V Institute of Oceanology, Chinese Academy of Sciences, Key Laboratory of Ocean Circulation and Wave, CAS, Qingdao 266071, China Graduate School of the Chinese Academy of Sciences, Beijing 100039, China%Institute of Oceanology, Chinese Academy of Sciences, Key Laboratory of Ocean Circulation and Wave, CAS, Qingdao 266071, China%Bedford Institute of Oceanography, Dartmouth, NS, Canada  | 
| Subjects | |
| Online Access | Get full text | 
| ISSN | 0254-4059 2096-5508 1993-5005 1993-5005 2523-3521  | 
| DOI | 10.1007/s00343-009-0112-1 | 
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| Summary: | A new model is proposed to estimate the significant wave heights with ERS-1/2 scatterometer data. The results show that the relationship between wave parameters and radar backscattering cross section is similar to that between wind and the radar backscattering cross section. Therefore, the relationship between significant wave height and the radar backscattering cross section is established with a neural network algorithm, which is, if the average wave period is 〈7s, the root mean square of significant wave height retrieved from ERS- 1/2 data is 0.51 m, or 0.72 m if it is 〉7s otherwise. | 
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| Bibliography: | significant wave height 37-1150/P neural networks scatterometer; significant wave height; neural networks; wind waves; swell wind waves P731.22 swell scatterometer TN951 ObjectType-Article-1 SourceType-Scholarly Journals-1 content type line 14 ObjectType-Feature-2 content type line 23  | 
| ISSN: | 0254-4059 2096-5508 1993-5005 1993-5005 2523-3521  | 
| DOI: | 10.1007/s00343-009-0112-1 |