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引用次数: 14
摘要
目前在苏格兰北部法罗-设得兰海峡东南边缘进行的观测，已与水文测量一起用于调查“大西洋”水向大陆架的转移。虽然海流主要平行于底部轮廓线，但观测结果表明，在陆架断裂处，通过从西南方向沿航道传播的扰动可以产生约2 cm s- 1的跨坡海流。
Flow across the continental slope off northern Scotland
Current observations at the southeastern edge of the Faroe-Shetland Channel, north of Scotland, have been used along with hydrographic measurements to investigate the transfer of ‘Atlantic’ water on to the continental shelf. Although currents are predominantly parallel to the bottom contours, the observations suggest that cross-slope currents of about 2 cm s−1 can be generated at the shelf break by disturbances propagating along the channel from the southwest.
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