Arctic Ocean deep water masses in the western Iceland Sea
Arctic Ocean deep water masses in the western Iceland Sea
复制标题
冰岛海西部的北冰洋深水团
DOI：
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发表时间：
1996
期刊：
影响因子：
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通讯作者：
Stefán S. Kristmannsson
中科院分区：
文献类型：
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作者：
E. Buch;S. Malmberg;Stefán S. Kristmannsson
冰岛-丹麦对国际格陵兰海项目的贡献是专门研究西冰岛海水团的分布和迁移。1987 ~ 1991年，每年9月，在格陵兰岛以东丹麦海峡以南至72°30′N的海域进行了温盐观测。数据显示，冰岛海西部的深水柱被一些略有不同的水团占据，这些水团都可以追溯到北冰洋的一个地层。特别值得注意的是，在某些年份，几乎未被稀释的欧亚盆地深水可以在远至丹麦海峡的南部观测到。
The Icelandic-Danish contribution to the international Greenland Sea Project was devoted to a study of the distribution and transport of water masses in the Western Iceland Sea. Each year in September from 1987 to 1991, temperature and salinity were observed on a station net in the area off east Greenland from the Denmark Strait in the south to 72°30′N. The data reveal that the deep water column of the western Iceland Sea is occupied by a number of slightly different water masses, which all can be traced back to a formation in the Arctic Ocean. It is especially noticeable that in some years almost undiluted Eurasian Basin Deep Water can be observed as far south as the Denmark Strait.