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2017
DOI: 10.1016/j.ocecoaman.2016.10.002
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Influence of flushing and other characteristics of coastal lagoons using data from Ghana

Abstract: The challenges associated with managing systems of shallow coastal lagoons along a rapidly evolving coastline are illustrated in a case study of small lagoon systems in Ghana where these important structures are relied on by a range of different stakeholders for a variety of different purposes including fishing, tourism and salt production. Results of some water quality measurements are presented, showing that these lagoons have poor ecological status where they experience either a lack of flushing by the tide… Show more

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Cited by 18 publications
(14 citation statements)
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“…The spring decrease in the water salinity in the Eastern basin of the Lake Saki may be due to both atmospheric precipitation and flood; in this area, the precipitation usually increases in the spring months. Similar seasonal phenomena in salinity fluctuations were also observed in other hy- persaline lakes (Geldenhuys et al, 2016;Mitchell et al, 2017). At the same time, there were interannual variability of the water salinity of the lake.…”
Section: Discussionsupporting
confidence: 81%
“…The spring decrease in the water salinity in the Eastern basin of the Lake Saki may be due to both atmospheric precipitation and flood; in this area, the precipitation usually increases in the spring months. Similar seasonal phenomena in salinity fluctuations were also observed in other hy- persaline lakes (Geldenhuys et al, 2016;Mitchell et al, 2017). At the same time, there were interannual variability of the water salinity of the lake.…”
Section: Discussionsupporting
confidence: 81%
“…The significant wave height along the coast is reported to be 1.2m (Wellens-Mensah et al 2002). The average tidal range along the coast of Ghana was estimated to be about 1m (Boateng 2012a;Mitchell, Boateng and Couceiro 2016).…”
Section: Accepted Manuscriptmentioning
confidence: 99%
“…The tidal range in the Gulf of Guinea is relatively low at 1-2 m, though storm surges are common (Boateng 2012a). The tidal range in Ghana is low and varies little between spring tide (1.32 m) and neap tides (0.58 m) (Mitchell, Boateng, and Couceiro 2017) and therefore have less influence on coastal processes except within tidal inlets. As a result, coastal lagoons in Ghana are either closed or open to the sea.…”
Section: Study Areamentioning
confidence: 99%
“…As a result, coastal lagoons in Ghana are either closed or open to the sea. While some are permanently closed to the sea, others are seasonally open to the sea (Mitchell, Boateng, and Couceiro 2017). Figure 1 shows the type (open or close) of sampled lagoons and their catchment sizes.…”
Section: Study Areamentioning
confidence: 99%