“…), because they can provide more spatial and temporal detail . 25 Analytical models are also widely used, such as Prandle (1981), Savenije (1986Savenije ( , 1989Savenije ( , 1993aSavenije ( , 2005Savenije ( , 2012Savenije ( , 2015, Lewis and Uncles, 2003, Gay and O" Donnell (2007), Kuijper and Van Rijn (2011), Aertsl et al, (2000), Brockway et al, (2006), Nguyen and Savenije (2006), Nguyen et al, (2008aNguyen et al, ( , 2008b, Cai et al, (2015a), Gisen et al, (2015a), Gisen et al, (2015b), Xu et al, (2015). These tools are based on the steady-state conservation of mass equation which indicates that the dispersive and advective transports of salt are in equilibrium and the effective longitudinal dispersion coefficient incorporates all 30 mixing mechanisms, where the dispersion coefficient along the estuary axis is either constant (e.g., Gay and O"Donnell, 2007) or variable (e.g., Van der Burgh, 1972;Savenije, 1986).…”