1992
DOI: 10.1016/0198-0149(92)90075-5
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Hydrographic indications of advection/convection effects in the Gulf of Elat

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Cited by 99 publications
(88 citation statements)
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“…In the summer, a photic layer with a continuous thermocline (surface temperature . 26uC), overlies a thermally homogeneous (20.6uC) deep waters (Wolf-Vecht et al 1992;Post et al 2011). During this period, dissolved inorganic N concentrations in the upper 100 m are at or below the detection limit, and Prochlorococcus dominates the phytoplankton community (Lindell and Post 1995).…”
Section: Methodsmentioning
confidence: 99%
See 1 more Smart Citation
“…In the summer, a photic layer with a continuous thermocline (surface temperature . 26uC), overlies a thermally homogeneous (20.6uC) deep waters (Wolf-Vecht et al 1992;Post et al 2011). During this period, dissolved inorganic N concentrations in the upper 100 m are at or below the detection limit, and Prochlorococcus dominates the phytoplankton community (Lindell and Post 1995).…”
Section: Methodsmentioning
confidence: 99%
“…1820 m deep waterbody (Wolf-Vecht et al 1992). It is subject to an annual cycle of stable summer stratification and deep winter mixing (Genin et al 1995;Post et al 2011).…”
Section: Methodsmentioning
confidence: 99%
“…During the summer months atmospheric dry deposition is a signiWcant source of nutrients to the euphotic zone, supporting transient phytoplankton blooms (Chen et al 2007;Paytan et al 2009). Beginning in the fall, cooling of surface waters initiates convective mixing, and a deeply mixed (300 m or more) water body is observed by winter (Wolf-Vetch et al 1992). Nutrients entrained from depth as a consequence of this mixing result in mesotrophic conditions (Lindell and Post 1995), with productivity likely limited by light (Labiosa et al 2003).…”
Section: Introductionmentioning
confidence: 99%
“…This causes a long residence time for water in the Gulf, with the surface water resident for one year and deeper waters between 3 and 8 years (Reiss & Hottinger, 1984), and combined with a lack of drainage into the straits results in a body of water that although coastal in geographical terms is representative of open ocean water in terms of its nutrient status (Klinker et al, 1976;Wolfvecht et al, 1992). There is a distinct seasonal pattern to the circulation of water in the Gulf, which is characterized by strati¢cation of the water column in the summer months, which disappears and by winter the water column is mixed as nutrient-rich water has risen to the surface (Klinker et al, 1976;Wolfvecht et al, 1992). The Synechococcus and Prochlorococcus community within the Gulf of Aqaba has previously been studied in detail (Fuller et al, 2003(Fuller et al, , 2005.…”
Section: Introductionmentioning
confidence: 99%