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At the time of the survey a small anticyclonic eddy of Atlantic Water was situated just offshore of the boundary current. The data suggest that the feature was recently detached from the boundary current, and, due to compensating effects of temperature and salinity on the thermal wind shear, ...
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The distributions and transports of deepwater masses at the western boundary in the tropical Atlantic off Brazil have been studied on three surveys along 35°W and 5°S and one at 10°S. Transports are obtained from direct measurements of the velocity fields (Pegasus profiling system and lowered...
Oscillatoria augustissimaPeaReduces the use of chemical fertilizers by 50% Improved nutritional value of pea seeds[58] Scenedesmus quadricaudaPeaIncreased protein, chlorophyll, and carotenoid content Better enzymatic activities in the leaves[59]
To achieve such density, the river water needs to have suspended sediment concentrations at least ∼ 35–45 kgm− 3, depending on the salinity and temperature of the ambient ocean water, to be able to plunge (Khan et al., 2005; Mulder and Syvitski, 1995). Hyperpycnal flows can ...
In the western Atlantic, the current’s deep-blue water, with its higher temperature and salinity, is readily distinguishable from surrounding waters, particularly along its well-defined western margin. The eastern edge gradually moves seaward as the current moves northward. The water between the cur...
For this study, we used approximately 14.5-year-long (January 2005–June 2019) three-dimensional daily outputs of temperature, salinity, and horizontal velocity fields in a domain of 3°–18° N and 124°–133° E. 2.2. Methods To remove high-frequency signals, such as tidal current and ...
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an eight‐mooring array of current meters and temperature/salinity sensors was installed across the CGFZ between 500 m and the sea floor to measure the mean transport of westward‐flowing Iceland‐Scotland Overflow Water (ISOW) and investigate the impact of the eastward‐flowing North Atlantic Cur...