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Analytical approach for predicting fresh water discharge in an estuary based on tidal water level observations

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Figure

Table 1, whereThe dependent dimensionless variables are also shown in δ is the damping number (a dimensionlessdescription of the increase, 0, or decrease, 0, of the
Table 2. Analytical solutions for tidal dynamics accounting for river discharge (Cai et al., 2014).
Figure 3. Sketch of the Yangtze estuary in China.
Figure 5. Comparison between analytically computed monthly averaged values (left-hand vertical scale: tidal amplitude; right-hand verticalscale: residual water level) and observations in the Yangtze estuary in 2005.
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