2013
DOI: 10.1016/j.csr.2013.04.038
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Tidal hydrodynamics in a two-inlet coastal lagoon in the Gulf of California

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Cited by 22 publications
(12 citation statements)
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“…In this vein, the wellknown categorisation of Kjerfve (1986) has helped to forge a better understanding of the different types of lagoons and how these respond over different time scales to different hydrological and geomorphological processes. Second, of interest to many researchers are the fundamental processes connected with the hydrodynamics and related water quality within the lagoon (Jewell et al, 2012;Dussaillant et al, 2009;Serrano et al, 2013). In deeper lagoons vertical density stratification can also be a consideration in the trapping or release of chemical species in deeper waters (Albarakati & Ahmad, 2012).…”
Section: Introductionmentioning
confidence: 99%
“…In this vein, the wellknown categorisation of Kjerfve (1986) has helped to forge a better understanding of the different types of lagoons and how these respond over different time scales to different hydrological and geomorphological processes. Second, of interest to many researchers are the fundamental processes connected with the hydrodynamics and related water quality within the lagoon (Jewell et al, 2012;Dussaillant et al, 2009;Serrano et al, 2013). In deeper lagoons vertical density stratification can also be a consideration in the trapping or release of chemical species in deeper waters (Albarakati & Ahmad, 2012).…”
Section: Introductionmentioning
confidence: 99%
“…Examples of such embayments are the Western Wadden Sea in the Netherlands, with the Marsdiep and Vlie inlets (e.g. Ridderinkhof 1988, also considered here), the Laguna de Términos in México (David and Kjerfve 1998) and the Santa María La Reforma in California (Serrano et al 2013).…”
Section: Introductionmentioning
confidence: 99%
“…They noted that fine sediments (silt and clay) typically accumulate in areas with low hydrodynamic energy, whereas sandy sediments typically accumulate in high-hydrodynamic environments. Serrano et al (2013) observed that the SAMARE coastal lagoon system has two high hydrodynamic energy zones, one in the north (Perihuete mouth) and one more in the south (Yameto mouth). The SAMARE coastal lagoon also has a low-energy zone (dominated by friction) in the central region of the system, which is mainly influenced by shallow waters.…”
Section: Resultsmentioning
confidence: 97%