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However, differences between the simulations were small and non-MultiGaussian riverbed properties seem to be of less importance for subsurface flow than non-MultiGaussian aquifer properties.
The sea surface temperature differences between the simulations using the uncoupled and coupled models are shown in Figure 11.
To reduce the systematic error, no absolute values were used to draw any conclusions, and only the differences between the simulations were considered.
In addition, we define the maximum mismatch as the maximum value of absolute differences between the simulations and the analytical results.
Therefore, we compared the horizontal simulated sea surface temperature distributions (Figure 10f,g,h,i,j) and the differences between the simulations using the uncoupled and coupled models (Figure 11) with those for the TRMM/TMI sea surface temperatures (Figure 3e,f,g,h), and the differences between before and after the typhoon had passed (Figure 3i,j,k,l).
Some differences between the simulations and the empirical data are found.
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The graph represents the salinity differences between the simulation with the source and without.
Compared the results with available experimental and numerical data conducted by Weber, they share the same trends though there are differences between the simulation and the experimental results, and the comparisons validate the effectiveness of the model and method.
Due to subgrid variability and differences between the simulation and observation scale (the Digital Elevation Model pixel versus the point measurement), the point-to-point comparison between observations and simulations shows a poor correlation.
Differences between the simulation and measurement results were due to inaccuracy of sensor alignment because crosstalk is sensitive to the sensor geometry.
Nevertheless, the substrate exhibits some roughness at the smallest scales, and evaporation causes the resurgence of the underlying substrate roughness, which explains the differences between the simulation and the experimental Mq curves.
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