中国第28次南极科学考察中的物理海洋观测  

Physical Oceanographical Observation in the 28th Chinese Antarctic Research Expedition

作　　者：连展[1,2] 乔方利[1,2] 魏泽勋[1,2] 王海员[1,2] 冯颖[1,2] 杨效东[1,2] 高立宝[1,2] 

机构地区：[1]国家海洋局第一海洋研究所,山东青岛266061 [2]海洋环境科学和数值模拟国家海洋局重点实验室,山东青岛266061

出　　处：《海洋科学进展》2013年第3期415-428,共14页Advances in Marine Science

基　　金：南北极环境综合考察与评估专项--2012年度南极周边海域物理海洋和海洋气象考察(CHINARE2012-01-01);极地对全球和我国气候变化影响的综合评价(CHINARE2012-04-04)

摘　　要：介绍了中国第28次南极科学考察中物理海洋部分的观测情况,包括航次站点位置、观测方式、观测内容、仪器设备和部分观测结果。整个航次顺利完成了预定工作内容,获得的数据可反映出观测海区的水团、环流等海洋特性。数据初步分析显示:南极半岛海域存在明显逆温层,普里兹湾P1断面观测时段可能不存在底层水下沉。Physical oceanographical observations carried out in the 28th Chinese Antarctic Research Expedi- tion are introduced, which include the locations of stations, the methods and contents of observations, in- struments and some of the results. This cruise finished all the tasks successfully. The obtained data can reflect the characteristics of the observed area, such as water mass, circulation currents and so on. The preliminary analysis of the data shows that there is an obvious temperature inversion layer in the sea area of Antarctica Peninsula, and no sinking of bottom water was possibly present in the Prydz Bay during the ob- servation along Section P1.

关 键 词：中国28次南极大洋考察 物理海洋 观测 

分 类 号：P728[天文地球—海洋科学] P732