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ZHANG Xin-ling, GUO Xin-shun, WU Zeng-mao, YOU Jian-hua, YAN Li-feng. The observation analyses and calculation method studies of solar irradiation at sea surface for the Bohai Sea[J]. Haiyang Xuebao, 2001, 23(2): 46-51.
Citation:
ZHANG Xin-ling, GUO Xin-shun, WU Zeng-mao, YOU Jian-hua, YAN Li-feng. The observation analyses and calculation method studies of solar irradiation at sea surface for the Bohai Sea[J]. Haiyang Xuebao, 2001, 23(2): 46-51.
ZHANG Xin-ling, GUO Xin-shun, WU Zeng-mao, YOU Jian-hua, YAN Li-feng. The observation analyses and calculation method studies of solar irradiation at sea surface for the Bohai Sea[J]. Haiyang Xuebao, 2001, 23(2): 46-51.
Citation:
ZHANG Xin-ling, GUO Xin-shun, WU Zeng-mao, YOU Jian-hua, YAN Li-feng. The observation analyses and calculation method studies of solar irradiation at sea surface for the Bohai Sea[J]. Haiyang Xuebao, 2001, 23(2): 46-51.
Analyzed are the observations(24 September to 7 October 1998,28 April to 11 May 1999) of daily solar irradiation of the Bohai Sea area and cloud.It is found that the daily solar radiation of the Bohai Sea area in spring is much greater than in autumn,and the difference of clear-day solar radiation between the observed and the theoretically calculated results in autumn is greater than in spring.It is thought that the development of something like cloud and fog resulted from the vertical transportation of sea surface moisture is the main cause.Moreover,the daily solar radiation of the Bohai Sea is calculated by an empirical formulation mainly based on cloud parameters.There is a relatively good consistency between the observation and the calculation results.It indicates that the calculation method and the parameters used in the for mulation are suitable for calculating the daily solar radiation of the Bohai Sea area in spring and autumn.
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