Observations of Tidal Headland Eddies in Deep Water

提出了一种三管齐下的野外研究方法来研究峡湾潮汐产生的侧壁涡流的产生、释放和消散。深（分层）水邻近的岬角，在那里产生涡流排除了立即消散的底部摩擦。室内实验表明，长寿命的涡流促进不同的特征流场比在较浅的环境中观察到。这一假设将得到验证。

MacCready0099058A three-pronged field effort is proposed to study the generation, release, and dissipation of tidally generated sidewall eddies in a fjord. The deep (stratified) water adjacent to the headland at which the eddy is generated precludes immediate dissipation by bottom friction. Laboratory experiments suggest that the long lifetime of the eddy promotes different characteristic flow fields than observed in shallower environments. This hypothesis will be tested.