North sea interaction with the north atlantic ocean
North sea interaction with the north atlantic ocean
复制标题
北海与北大西洋的相互作用
DOI：
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发表时间：
1997
期刊：
影响因子：
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通讯作者：
J. Huthnance
中科院分区：
文献类型：
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作者：
J. Huthnance
关于平均汇率的证据进行审查，占主导地位的总流入量和1.7 × 106米3秒-1的各种路线的北方北海。审查了可能的贡献过程。它的结论是，在大陆架边缘的地形约束放松强摩擦和大的变化在短时间尺度上，都与强大的潮汐和风力驱动的苏格兰周围的流动。有迹象表明，北海环流是由北大西洋场控制，迫使苏格兰周围和大西洋-北海盐度差异：这些值得进一步调查。
Evidence is reviewed regarding the average rates of exchange, dominated by a total inflows & 1.7 x 106 m3s-1 by various routes to the northern North Sea. Possible contributory processes are reviewed. It is concluded that the topographic constraint at the shelf edge is relaxed by strong friction and large variability on short time-scales, both associated with strong tidal and wind-driven flows around Scotland. There are suggestions that the North Sea circulation is controlled by North Atlantic fields, forcing around Scotland and Atlantic — North Sea salinity differences: these warrant further investigation.