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本文讨论了南黄海北部海域及青岛近海海水激光(6328A)衰减系数的垂直分布与温跃层的相关性。依据三个年度不同季节(春、夏、秋)现场实测结果,叙述了衰减系数垂直分布的季节变化,并对现场测量方法提出了改进方案。 一、本海域的水文特征 观测海域的温、盐结构随季节变化。冬季诸月(12—3月)由于海面冷却和蒸发所致的对流混合达到海底,海水温、盐分布呈垂直均匀或接近垂直均匀状态,夏半年(5—10月)
This paper discusses the correlation between the vertical distribution and the thermocline of the attenuation coefficient of the North Yellow Sea and Qingdao offshore sea lasers (6328A). According to the field measurement results in different seasons (spring, summer and autumn) in each of the three years, the seasonal variation of the vertical distribution of the attenuation coefficient is described and an improved scheme is proposed for the field measurement method. First, the hydrological characteristics of the sea The temperature and salt structure of the sea area under observation changes with the seasons. In the winter months (December-March), convection caused by sea surface cooling and evaporation reached the seafloor. The temperature and salinity of seawater reached a vertical or even vertical distribution. During the summer half year (May-October)