高度分层的南部非洲河口的环流

J. Largier, J. Slinger
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引用次数: 14

摘要

摘要:本文以非洲南部河口为例,回顾了高度分层条件下河口环流的性质,这些河口面积小,与海洋的联系有限。虽然重点是一般的水动力过程和特征,但注意到从特定河口的实地观测作为说明这些过程和特征的一种方式。其显著特征是潮侵锋、底密度流和河口上游长居深水。解释这些特征的重要水动力过程是河口交换的内部水力控制、浮力驱动的海水向陆地侵入、向上剪切驱动的夹带和退潮流出。通过对原型的季节变化的讨论和对在其他南部非洲河口观察到的这些特征的讨论,解决了这些过程和特征预期发生的背景。区别在于……
本文章由计算机程序翻译,如有差异,请以英文原文为准。
CIRCULATION IN HIGHLY STRATIFIED SOUTHERN AFRICAN ESTUARIES
Summary The nature of estuarine circulation under highly stratified conditions is reviewed in the context of southern African estuaries that are small and have a constricted connection to the ocean. While the focus is on the generic hydrodynamic processes and features, attention is given to field observations from a particular estuary as a way of illustrating these processes and features. Notable features are the tidal intrusion front, the bottom density current and the long-residence deep water in the upper estuary. The important hydrodynamic processes, which account for these features, are internal hydraulic control of exchange through the mouth, buoyancy-driven landward intrusion of sea water, upward shear-driven entrainment and ebb tidal outflow. The context in which these processes and features are expected to occur is addressed through a discussion of seasonal variations in the prototype and through a discussion of these features observed in other southern African estuaries. A distinction is made be...
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