| 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].Acta Oceanologica Sinica,1988,(3):402-411 |
| The features of temporal variation and the distribution of dissolved oxygen in the western Taiwan Strait |
| The features of temporal variation and the distribution of dissolved oxygen in the western Taiwan Strait |
| 投稿时间：1987-08-10 修订日期：1988-01-30 |
| DOI： |
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| 英文关键词: |
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| 作者 | 单位 | | Yi Ruizao | Third Institute of Oceanography, State Oceanic Administration, Xiamen, China | | Lin Jianyun | Third Institute of Oceanography, State Oceanic Administration, Xiamen, China | | Lu Meiluan | Third Institute of Oceanography, State Oceanic Administration, Xiamen, China | | Wang Weiqiang | Third Institute of Oceanography, State Oceanic Administration, Xiamen, China | | Huang Shanggao | Third Institute of Oceanography, State Oceanic Administration, Xiamen, China |
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| 中文摘要: |
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:
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. |
| 英文摘要: |
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:
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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