一幅新的迎风航道测深图

William G. Metcalf , Marvel C. Stalcup
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引用次数: 2

摘要

位于古巴东端和海地西北端之间的海底脊形成了向风通道的基底,是大西洋深水和加勒比海西北部开曼盆地深水之间的地形屏障。利用精密雷达测距系统进行的水深测量显示,该山脊的控制深度为1560米。结果与先前基于温度分布和水深测量的估计一致。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
A new bathymetric chart of the Windward Passage sill

The submarine ridge between the eastern tip of Cuba and the northwestern tip of Haiti forms the sill of the Windward Passage and is the topographic barrier between the deep water of the Atlantic Ocean and that of the Cayman Basin in the northwestern Caribbean Sea. The controlling depth of this ridge was shown to be 1560 m by a bathymetric survey using a precision radar ranging system.The results agree with previous estimates based on temperature distribution and bathymetric surveys.

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