Current System in the Northern Irish Sea

Current System in the Northern Irish Sea
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北爱尔兰海的海流系统

DOI:
10.1038/224059a0
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发表时间:
1969
期刊:
影响因子:
64.8
通讯作者:
H. W. Hill
H. W. Hill
中科院分区:
综合性期刊1区
文献类型:
--
作者:
J. Ramster;H. W. Hill

文献摘要

被引文献

相似文献

在过去的四年里,对北爱尔兰海的潮汐流进行了天气性的直接测量,测量范围很广,覆盖了水柱上的各个点。在进行这些研究之前,海洋环流主要是根据表面温度和盐度图、表面漂流瓶的运动以及考虑各种参数的连续性方程而得出的一些相当广泛的水输送估计进行定性推断。
IN the past four years direct measurements of the tidal streams in the northern Irish Sea have been made synoptically over an extensive area and at various points in the water column. Before these studies, the circulation of the sea was largely a matter of qualitative deduction, based on surface temperature and salinity charts, the movement of surface drift bottles and a few rather broad-based estimates of water transport derived from consideration of the continuity equations for a variety of parameters1.