2007
DOI: 10.1007/s10872-007-0038-1
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Dynamics of estuarine residual circulation in a narrow channel including tidal-nonlinear effects

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Cited by 3 publications
(2 citation statements)
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“…The weak residual flow during the dry season can be explained by tidal straining (Burchard et al, 2014;Geyer and MacCready, 2014). Several authors have shown that estuarine residual circulation weakens when tidal importance increases (Li, 1997;Shiraki and Yanagi, 2007;Cheng et al, 2011) as is the case in the Bons Sinais Estuary, where the tidal amplitude reaches ~ 4 m during spring tide.…”
Section: Discussionmentioning
confidence: 98%
“…The weak residual flow during the dry season can be explained by tidal straining (Burchard et al, 2014;Geyer and MacCready, 2014). Several authors have shown that estuarine residual circulation weakens when tidal importance increases (Li, 1997;Shiraki and Yanagi, 2007;Cheng et al, 2011) as is the case in the Bons Sinais Estuary, where the tidal amplitude reaches ~ 4 m during spring tide.…”
Section: Discussionmentioning
confidence: 98%
“…Real estuaries exhibit a range of mixing, however, with partially mixed conditions common in the upper estuary and well-mixed salinity near the mouth (Levasseur, Shi et al 2007). The circulation is further complicated by lateral mixing (Nidzieko, Hench et al 2009), the tidal cycle (Nakayama, Okada et al 2005;Guo and Valle-Levinson 2007;Shiraki and Yanagi 2007;Stacey, Fram et al 2008), freshwater inflow (Yanagi and Shimomura 2006), and long-term meteorological variability (Aoki and Isobe 2006). The interaction of these processes also produces estuaries that have higher salinities than ocean values (reverse estuaries) and net inflow from the ocean (storage estuaries).…”
Section: Introductionmentioning
confidence: 99%