2020
DOI: 10.1016/j.marchem.2020.103806
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Dissolved oxygen dynamics in Ria Formosa Lagoon (South Portugal) - A real time monitoring station observatory

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Cited by 19 publications
(12 citation statements)
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“…A significant positive correlation was found between temperature and salinity (r = 0.1715; p( uncorr ) = 0). Regarding DO, an inverse relationship was found with temperature (r = −0.1745; p( uncorr ) = 0) and salinity (r = −0.2887; p( uncorr ) = 0) and this is in accordance with the literature which states that an increase in water temperature and salinity decreases DO solubility [35,59,84], whereas a positive correlation was found with pH (y = 1.4673 × −4.8995; r = 0.1897; p( uncorr ) = 0), likely due to the decrease in CO 2 during photosynthetic processes that increase both DO and pH. Finally, it was found a significant inverse relationship with mean depth (r = −0.5242; p( uncorr ) = 0.0020),…”
Section: Dissolved Oxygensupporting
confidence: 90%
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“…A significant positive correlation was found between temperature and salinity (r = 0.1715; p( uncorr ) = 0). Regarding DO, an inverse relationship was found with temperature (r = −0.1745; p( uncorr ) = 0) and salinity (r = −0.2887; p( uncorr ) = 0) and this is in accordance with the literature which states that an increase in water temperature and salinity decreases DO solubility [35,59,84], whereas a positive correlation was found with pH (y = 1.4673 × −4.8995; r = 0.1897; p( uncorr ) = 0), likely due to the decrease in CO 2 during photosynthetic processes that increase both DO and pH. Finally, it was found a significant inverse relationship with mean depth (r = −0.5242; p( uncorr ) = 0.0020),…”
Section: Dissolved Oxygensupporting
confidence: 90%
“…In addition, field work also disturbs natural ecosystems such as the Marano and Grado Lagoon. The use of permanent sampling equipment (i.e., anchored stations, surface floating modules or buoys) is a helpful approach to investigate DO level oscillations with low sampling time interval (from minutes to hours) and to cover the natural day/night cycles [31][32][33][34][35].…”
Section: Introductionmentioning
confidence: 99%
“…The YSCWM is vertically stratified in summer and lacks substantial vertical exchange between cold bottom‐waters and the upper mixed layer due to the strong thermocline. Therefore, dissolved oxygen is generally low due to the weak currents during neap tides and high due to the strong currents during spring tides (Casila et al., 2019; Cravo et al., 2020; Gale et al., 2006).…”
Section: Discussionmentioning
confidence: 99%
“…10.1029/2020JC016696 9 of 16 upper mixed layer due to the strong thermocline. Therefore, dissolved oxygen is generally low due to the weak currents during neap tides and high due to the strong currents during spring tides (Casila et al, 2019;Cravo et al, 2020;Gale et al, 2006).…”
Section: Time Lag Between Hydrodynamic Processes and Pacific Cod Growthmentioning
confidence: 99%
“…Clams were divided into four 250 L recirculated water systems (RAS), equipped with a filtration system and a UV-c unit (25 W UV-c, 6.000 µW s/cm 2 ) and a temperature control unit (composed of a 300-W submergible heater and a 1 2 HP chiller, controlled by a thermostat), with similar salinity (35 ± 1), but different water temperatures (10, 15, 20 and 25 • C). This range of temperatures is representative of the seasonal fluctuations in water temperature to which clams are being subject in recent years at Ria Formosa [52], simulating, at the same time, temperature shifts as occurs during extreme weather events. R. decussatus individuals were let to acclimate to the different temperatures for 24 h. After this period, clams were moved to experimental RAS and divided into two treatments: (I) tanks at 10, 15, 20 and 25 • C water temperature in the absence of MWCNTs-COOH contamination; (II) tanks at 10, 15, 20 and 25 • C in the presence of MWCNTs-COOH (0.01 mg/L).…”
Section: Sampling and Laboratory Conditionsmentioning
confidence: 99%