1996
DOI: 10.1006/ecss.1996.0016
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Transient Coastal Upwelling and Water Circulation in Bantry Bay, a Ria on the South-west Coast of Ireland

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Cited by 32 publications
(22 citation statements)
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“…Most of the bay averages 30 m in depth, increasing to 70 m near the mouth. Throughout the summer, cyclical coastal upwelling in the bay has been known to drive the development of toxic algal blooms, with shelf waters intruding into the bay on the relaxation of upwelling (Edwards et al 1996). The northern site in Clifden Bay, Connemara (northwest Ireland), is in comparison, a relatively sheltered, shallow bay (maximum depth ~14 m) only 9 km in length.…”
Section: Methodsmentioning
confidence: 99%
“…Most of the bay averages 30 m in depth, increasing to 70 m near the mouth. Throughout the summer, cyclical coastal upwelling in the bay has been known to drive the development of toxic algal blooms, with shelf waters intruding into the bay on the relaxation of upwelling (Edwards et al 1996). The northern site in Clifden Bay, Connemara (northwest Ireland), is in comparison, a relatively sheltered, shallow bay (maximum depth ~14 m) only 9 km in length.…”
Section: Methodsmentioning
confidence: 99%
“…Circulation is thus primarily wind driven; this is also due to the fact that the bay is axially aligned to the predominant wind direction from the southwest (Edwards et al, 1996). When the bay is thermally stratified, variations in wind direction cause two layer oscillatory flows which generally result in the import of water from the near coastal continental shelf containing phytoplankton (Edwards et al 1996), and in general water flushing is in an anticlockwise direction, which has implications for nutrient availability for shellfish culture. Substantial mixing due to this wind driven exchange then prevents any one phytoplankton species dominating the bay (Raine et al, 1993).…”
Section: Study Sitementioning
confidence: 99%
“…It should be noted that in the ADCP current meter was deployed at 40 m depth in the study of the Carter et al, 1979;Walters and Gartner, 1985;Valle Levinson et al, 1998;Wong and Moses-Hall, 1998;Wong and DiLorenzo, 1988;Wong, 2002). The effect of coastal winds is specially relevant in areas affected by permanent or seasonal upwelling, as it is the case of the Galician rías (Rosón et al, 1997;Álvarez-Salgado et al, 2000;Pardo et al, 2001), the Chilean fjords (Aysen Fjord, Cáceres et al, 2002) or Bantry Bay in South West Ireland (Edwards et al, 1996). Similarly high percentages of the subtidal current variability explained by coastal winds have been found in the Ría de Vigo (>65%; Piedracoba et al, 2005), the Ría de Arousa (50%; Rosón et al, 1997) (Rosón et al, 1997;Álvarez-Salgado et al, 2000).…”
Section: Subtidal Circulation Patternsmentioning
confidence: 99%