{"title":"CIRCULATION IN HIGHLY STRATIFIED SOUTHERN AFRICAN ESTUARIES","authors":"J. Largier, J. Slinger","doi":"10.1080/10183469.1991.9631317","DOIUrl":null,"url":null,"abstract":"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...","PeriodicalId":161337,"journal":{"name":"Southern African Journal of Aquatic Sciences","volume":"1 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"1991-06-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"14","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Southern African Journal of Aquatic Sciences","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1080/10183469.1991.9631317","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 14
Abstract
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...