Thus, hydrologic variability (e.g., inputs, water levels, depths), sediment-water interchange, and wind have greater effects than they do in deep, permanent, freshwater lakes.
In general, the water-level depth in the area ranges between 0.25 and 14.25 m from the ground level.
Hydrogeological parameters such as storativity, specific capacity, transmissivity, drawdown, pumping rate, static water level, total depth, and well yield were computed from well completion reports and aquifer test.
According to the presented results by Ayca (2012), it has been revealed that the tsunami generated at YAN, PIN, and CMN increases the water level, flow depth, and current velocities near Haydarpaşa Port, unlike tsunamis originating elsewhere.
Among these, the PIN and YAN are selected as critical sources that may cause tsunamis with higher water levels, flow depth, and strong current velocities at Yenikapı.
The new canal was 36 metres (117 feet) wide at water level, with a depth of 2 metres (6.5 feet).
In the end, the water level reached a depth of 4.46m, slightly lower than predicted and below the 5.45m reached in the 1974 flood.
According to Corey Brooks function, the saturation height function can be obtained by combining the height above the free water level, the reservoir depth and the pore throat size.
The areal coverage of submerged and floating-leaved aquatic vegetation (SAV) is determined by the potential habitat space available between the minimum water level and the depth of light penetration (i.e., the photic zone).
As expected, water level and well depth are location- and formation-specific.
