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| The features of temporal variation and the distribution of dissolved oxygen in the western Taiwan Strait | |
| 引用本文： | Yi Ruizao,Lin Jianyun,Lu Meiluan,Wang Weiqiang,Huang Shanggao. The features of temporal variation and the distribution of dissolved oxygen in the western Taiwan Strait[J]. 海洋学报(英文版), 1988, 7(3): 402-411 |
| 作者姓名： | Yi Ruizao Lin Jianyun Lu Meiluan Wang Weiqiang Huang Shanggao |
| 作者单位： | Third Institute of Oceanography, State Oceanic Administration, Xiamen, China;Third Institute of Oceanography, State Oceanic Administration, Xiamen, China;Third Institute of Oceanography, State Oceanic Administration, Xiamen, China;Third Institute of Oceanography, State Oceanic Administration, Xiamen, China;Third Institute of Oceanography, State Oceanic Administration, Xiamen, China |
| 摘 要： | The distribution of dissolved oxygen in the western Taiwan Strait was discussed by using the method of harmonic analysis. The periodic variation of dissolved oxygen in seawatcr can be expressed by the Fourier series:whereto is annual average value; Am andφm are amplitude and phase of constituent, respectively. The distribution of A0 and the annual and semiannual constants (Am, φm) of dissolved oxygen in the surface, bottom and vertical section of the western Taiwan Strait were described. The effect of the various currents on the distribution of dissolved oxygen was also discussed. |
| 收稿时间： | 1987-08-10 |
| 修稿时间： | 1988-01-30 |
The features of temporal variation and the distribution of dissolved oxygen in the western Taiwan Strait |
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| Yi Ruizao,Lin Jianyun,Lu Meiluan,Wang Weiqiang and Huang Shanggao. The features of temporal variation and the distribution of dissolved oxygen in the western Taiwan Strait[J]. Acta Oceanologica Sinica, 1988, 7(3): 402-411 | |
| Authors: | Yi Ruizao Lin Jianyun Lu Meiluan Wang Weiqiang Huang Shanggao |
| Affiliation: | Third Institute of Oceanography, State Oceanic Administration, Xiamen, China |
| Abstract: | The distribution of dissolved oxygen in the western Taiwan Strait was discussed by using the method of harmonic analysis. The periodic variation of dissolved oxygen in seawatcr can be expressed by the Fourier series: Y=A0+ΣM=1nAmcos(mωt-Φm), where A0 is annual average value; Am and φm are amplitude and phase of constituent, respectively. The distribution of A0 and the annual and semiannual constants (Am, φm) of dissolved oxygen in the surface, bottom and vertical section of the western Taiwan Strait were described. The effect of the various currents on the distribution of dissolved oxygen was also discussed. |
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