Application of the Hilbert-Huang Transform to the Estimation of Air-Sea Turbulent Fluxes
文献类型：期刊论文
| 作者 | Wang, Juanjuan1,2; Song, Jinbao1; Huang, Yansong3; Fan, Conghui1 |
| 刊名 | BOUNDARY-LAYER METEOROLOGY
 |
| 出版日期 | 2013-06-01 |
| 卷号 | 147期号:3页码:553-568 |
| 关键词 | Air-sea flux Eddy covariance Gap scale Hilbert-Huang transform |
| ISSN号 | 0006-8314 |
| 通讯作者 | Song, JB |
| 中文摘要 | The Hilbert-Huang transform (HHT) is applied to analyzing the turbulent time series obtained within the atmospheric boundary layer over the ocean. A method based on the HHT is introduced to reduce the influence of non-turbulent motions on the eddy-covariance based flux by removing non-turbulent modes from the time series. The scale dependence of the flux is examined and a gap mode is identified to distinguish between turbulent modes and non-turbulent modes. To examine the effectiveness of this method it is compared with three conventional methods (block average, moving-window average, and multi-resolution decomposition). The data used are from three sonic anemometers installed on a moored buoy at about 6, 4 and 2.7 m height above the sea surface. For each method, along-wind and cross-wind momentum fluxes and sensible heat fluxes at the three heights are calculated. According to the assumption of a constant-flux layer, there should be no significant difference between the fluxes at the three heights. The results show that the fluxes calculated using HHT exhibit a smaller difference and higher correlation than the other methods. These results support the successful application of HHT to the estimation of air-sea turbulent fluxes. |
| 英文摘要 | The Hilbert-Huang transform (HHT) is applied to analyzing the turbulent time series obtained within the atmospheric boundary layer over the ocean. A method based on the HHT is introduced to reduce the influence of non-turbulent motions on the eddy-covariance based flux by removing non-turbulent modes from the time series. The scale dependence of the flux is examined and a gap mode is identified to distinguish between turbulent modes and non-turbulent modes. To examine the effectiveness of this method it is compared with three conventional methods (block average, moving-window average, and multi-resolution decomposition). The data used are from three sonic anemometers installed on a moored buoy at about 6, 4 and 2.7 m height above the sea surface. For each method, along-wind and cross-wind momentum fluxes and sensible heat fluxes at the three heights are calculated. According to the assumption of a constant-flux layer, there should be no significant difference between the fluxes at the three heights. The results show that the fluxes calculated using HHT exhibit a smaller difference and higher correlation than the other methods. These results support the successful application of HHT to the estimation of air-sea turbulent fluxes. |
| WOS标题词 | Science & Technology ; Physical Sciences |
| 学科主题 | Meteorology & Atmospheric Sciences |
| 类目[WOS] | Meteorology & Atmospheric Sciences |
| 研究领域[WOS] | Meteorology & Atmospheric Sciences |
| 关键词[WOS] | EXCHANGE |
| 收录类别 | SCI |
| 原文出处 | 10.1007/s10546-012-9784-8 |
| 语种 | 英语 |
| WOS记录号 | WOS:000319475000009 |
| 公开日期 | 2014-07-17 |
| 源URL | [http://ir.qdio.ac.cn/handle/337002/16392]  |
| 专题 | 海洋研究所_海洋环流与波动重点实验室 |
| 作者单位 | 1.Chinese Acad Sci, Inst Oceanol, Qingdao, Peoples R China 2.Chinese Acad Sci, Grad Univ, Beijing, Peoples R China 3.South China Sea Marine Engn Surveying Ctr, State Ocean Adm, Guangzhou, Guangdong, Peoples R China |
| 推荐引用方式 GB/T 7714 | Wang, Juanjuan,Song, Jinbao,Huang, Yansong,et al. Application of the Hilbert-Huang Transform to the Estimation of Air-Sea Turbulent Fluxes[J]. BOUNDARY-LAYER METEOROLOGY,2013,147(3):553-568. |
| APA | Wang, Juanjuan,Song, Jinbao,Huang, Yansong,&Fan, Conghui.(2013).Application of the Hilbert-Huang Transform to the Estimation of Air-Sea Turbulent Fluxes.BOUNDARY-LAYER METEOROLOGY,147(3),553-568. |
| MLA | Wang, Juanjuan,et al."Application of the Hilbert-Huang Transform to the Estimation of Air-Sea Turbulent Fluxes".BOUNDARY-LAYER METEOROLOGY 147.3(2013):553-568. |
入库方式： OAI收割
来源：海洋研究所
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