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.
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Third Institute of Oceanography,State Oceanic AdministrationThird Institute of Oceanography,State Oceanic Administration
SHEN Junqiang
QIU Yun
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Third Institute of Oceanography,State Oceanic Administration
Laboratory for Regional Oceanography and Numerical Modeling,Qingdao National Laboratory for Marine Science and TechnologyThird Institute of Oceanography,State Oceanic Administration
QIU Yun
GUO Xiaogang
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Third Institute of Oceanography,State Oceanic AdministrationThird Institute of Oceanography,State Oceanic Administration
GUO Xiaogang
PAN Aijun
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Third Institute of Oceanography,State Oceanic AdministrationThird Institute of Oceanography,State Oceanic Administration
PAN Aijun
ZHOU Xiwu
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Third Institute of Oceanography,State Oceanic AdministrationThird Institute of Oceanography,State Oceanic Administration