2012
DOI: 10.1016/j.ecss.2012.05.017
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Dynamics of the Douro estuary sand spit before and after breakwater construction

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Cited by 40 publications
(27 citation statements)
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“…bathymetric survey performed by the IH. The sand spit topography was taken from a 2015 topographical survey [68], and the adjacent coastal bathymetry was obtained from the Bathymetric Model of Douro (IH). For both estuaries, additional ocean bathymetric data was extracted from the GEBCO database [69], and the different data sets considered were interpolated using a Kriging algorithm [70,71].…”
Section: A Portuguese Case Study: Douro and Minho Estuariesmentioning
confidence: 99%
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“…bathymetric survey performed by the IH. The sand spit topography was taken from a 2015 topographical survey [68], and the adjacent coastal bathymetry was obtained from the Bathymetric Model of Douro (IH). For both estuaries, additional ocean bathymetric data was extracted from the GEBCO database [69], and the different data sets considered were interpolated using a Kriging algorithm [70,71].…”
Section: A Portuguese Case Study: Douro and Minho Estuariesmentioning
confidence: 99%
“…It flows from the Sierra de Urbion, in Spain, to the Atlantic Ocean, in northern Portugal, ending in an urban estuary surrounded by two major cities: Porto and Vila Nova de Gaia (Figure 1). The Douro is a highly dynamic narrow estuary with torrential regimes that produce strong currents and recurrent severe floods that cause serious damage to the riverine populations and navigation problems [68,72]. Its dynamics is mainly forced by freshwater flows, being very dependent on highly variable natural conditions and on the hydropower production schedule of the Crestuma-Lever dam and of the other 50 national and international river basin dams.…”
Section: A Portuguese Case Study: Douro and Minho Estuariesmentioning
confidence: 99%
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“…Keberadaan mangrove berperan dalam memerangkap sedimen dan mempertahankan lokasi tersebut dari abrasi laut. Kondisi tersebut juga ditentukan oleh dominasi banjir akibat deformasi gelombang pasang, angin, pasokan sedimen dan transportasi sedimen, hidrodinamika serta perubahan dasar perairan (Bastos et al, 2012;Xie & Pan, 2012).…”
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