90年代胶州湾海域的温、盐结构  

Temperature and Salinity Structures of Jiaozhou Bay Waters During 1991～1995

作　　者：杨玉玲[1] 吴永成[1] 

机构地区：[1]中国科学院海洋研究所,青岛266071

出　　处：《黄渤海海洋》1999年第3期31-36,共6页Journal of Oceanography of Huanghai & Bohai Seas

摘　　要：本文分析了 １９９１～１９９５ 年间胶州湾 １０ 个测站所获海水温、盐度资料，结果表明：胶州湾水温场的空间结构分为冬季型和夏季型两种类型。水温的变化主要受太阳辐射、黄海水入侵及潮流的影响。盐度场的空间结构比温度场单纯，只存在一种类型。盐度变化主要受入海径流、降水、黄海水入侵及潮流的影响。This paper analyzes the temperature and salinity data acquired at 10 observation points in Jiaozhou Bay during 1991～1995 The results indicate that the spatial structure of the temperature field can be divided into two types: winter type and summer type. The variations in temperature result mainly from the effects of solar radiation, intrusion of the Yellow Sea water and tide. The spatial structure of the salinity field is simpler than that of the temperature field, having one type only . The variations in salinity result mainly from the effects of runoff emptying into sea, precipitation and intrusion of the Yellow Sea water and tide.

关 键 词：胶州湾 温度 盐度 海水 

分 类 号：P731.11[天文地球—海洋科学] P731.12