Currents and pressure records from the DeepLev mooring station (Eastern Levantine Basin) are analyzed to identify the dominant tidal constituents and their seasonal and depth variability. Harmonic and spectral analysis on seasonal segments of currents and pressure reveal attributes of the tidal regime in the Eastern Levantine Basin: (1) Dominant semidiurnal sea-level variability; (2) seasonal variation of semidiurnal and diurnal tides found in both currents and pressure datasets; and (3) significant diurnal currents with weak semidiurnal currents in all seasons. The most dominant tidal constituent found from the pressure dataset is the M2 (12.4 h). Results from pressure datasets generally agree with previous models and observations of semidiurnal tides, while the diurnal tides are larger than previously reported by 8-9 cm in the winter and 1-2 cm in the summer. The surface current variability differs from the one reported before in the Eastern Levantine Basin, with M2 magnitudes weaker by 1 cm, while the diurnal tides (K1, O1) are 1-2 cm larger. Seasonal segments showed seasonal differences in the local tidal regime’s amplitudes, with the K1 (7 cm difference between winter and fall) and S2 (4 cm difference between summer and fall) the most pronounced. We analyzed the M2 and S2 tides using surface drifters near DeepLev at different dataset lengths while considering the time constraints needed to resolve the tides adequately. The longer the dataset, the higher the resolution of the tidal analysis and the lower the amplitude leakages from nearby frequencies resulting in weaker tidal currents.

Phytoplankton bloom in the Gulf of Elat/Aqaba was studied before mainly using one-dimensional models and observations from the northern Gulf. Thus, the spatial variability within the Gulf and the contribution of physical processes such as horizontal advection to the bloom have not yet been studied. Moreover, various factors such as light limitation are still debated. Here we used a three-dimensional coupled physical-ecological model for the Gulf of Elat/Aqaba to study the mechanisms for phytoplankton bloom throughout the Gulf. We found the southern surface bloom to be higher than the northern surface. In contrast, southern integrated bloom is lower than the northern bloom. These differences are due to spatial variations in the mixed layer depth, which is much deeper in the northern Gulf compared with the south. Moreover, horizontal advection controls phytoplankton integrated biomass during the bloom, a process often neglected when dealing with phytoplankton blooms. Finally, we found that light limits growth of the northern integrated bloom.

The Gulf of Elat/Aqaba exhibits high inter-annual variability in mixed layer depth. Observations from the northern Gulf show differences of hundreds of meters in winter mixing depth, which ranges between 300 m in years with shallow mixing and up to 700 m in years with deep mixing. Deep mixing events can occur in two consecutive years or after four consecutive years of shallow mixing. The mixing depth has an effect on the concentration of nutrients and chlorophyll (and other tracers) in the surface and deep water. Using a 3D coupled physical-ecological model, we study the effect of shallow vs. deep mixing on the processes controlling the phytoplankton bloom and on nutrient accumulation in the deep water. We found that years with deep mixing are characterized by larger spatial variability in surface and integrated chlorophyll concentration during the mixing season. We also found that horizontal advection is more important for integrated phytoplankton concentration in years with deep mixing in the northern Gulf. Even when mixing was deep and nutrient limitation decreased, light limitation on growth was enhanced more in the north compared with the south. In addition, we showed that the nutrient accumulation in the deep water after a year with deep mixing of the northern Gulf was initially affected mostly by physical processes (such as advection and vertical mixing), and less from ecological regeneration and switched gradually to be dominated by ecological processes alone during the third year of shallow mixing.