Latitudinal displacements of the gulf-stream (1966 to 1977) and their relation to changes in temperature and zooplankton abundance in the ne atlantic
Latitudinal displacements of the gulf-stream (1966 to 1977) and their relation to changes in temperature and zooplankton abundance in the ne atlantic
复制标题
墨西哥湾流的纬度位移（1966年至1977年）及其与近大西洋温度和浮游动物丰度变化的关系
DOI：
--
复制
发表时间：
1980
期刊：
影响因子：
--
通讯作者：
J. Stephens
中科院分区：
文献类型：
--
作者：
Ah Taylor;J. Stephens
结果表明，1966~1971年间，墨西哥湾流北墙向南移动，1973年以后又向北移动。而与任何几个人都没有明确的关系！相关的风和..PTS：……当然，东北大西洋的海面温度、盐度和浮游动物丰度也有类似的趋势。因此，墨西哥湾流的移动是围绕北大西洋大部分地区的大规模变化的一部分。这些变化要么是全球大气环流变化的单独表现，要么是东北大西洋的变化是墨西哥湾流变化的间接结果。
lt is shown that the north wall of the Gulf Stream was displaced southward during 1966 to 1971 and returned north ward after 1973. While there was no clear relation with any of severa! relevant wind and .. PtS:.~~ ure i?dices, there were similar trends in sea-surface temperature, salinity and abundance-ofzooplankton in the NE Atlantic. The displacements of the Gulf Stream are therefore part of a large-scale change encompassing most of the North Atlantic. These changes are either separate manifestations of variations in the global atmospheric circulation, or the changes in the NE Atlantic are the indirect result of variations in the Gulf Stream.