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Maximum water surface temperature usually occurred at 16:00 h, and minimum at 06:00 h.
The maximum water surface change just upstream of a bridge is termed the afflux in hydraulic engineering.
Fig. 4 Estimated rupture parameters for each segment of each source YAN, PIN, and CMN (left) and initial sea state in Domain B a, distribution of arrival time of first wave in Domain B b, distribution of maximum water surface elevation in Domain B and Domain C c after YAN, PIN, and CMN simulations (depth refers to focal depth).
The spatial distribution of the maximum water surface level caused by storm surge is spatially limited to within the northwestern part of Leyte Gulf.
The mean error of predicted maximum water surface level was largest at 2.37 and 4.15 m in the no-data-assimilation cases of WRF and CReSS, respectively.
If the spatial distribution of the maximum water surface elevation can be obtained, it can be regarded for a proxy of validation for typhoon modeling.
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In an enclosed body of water, fetch is also defined as the distance between the points of minimum and maximum water-surface elevation.
The estimated errors of minimum central pressure by different configurations are 24 hPa maximum, but the maximum difference of water surface level is 4.42 m (Table 1).
Patterns of stratification reflected local weather conditions but also varied among ponds depending on their morphometric characteristics such as maximum water depth and surface area to perimeter ratio.
However, the maximum water height at the surface (0.8 m) is smaller than in the case of the larger source.
The comparison with the data available in literature showed that the results of the numerical simulation reproduce satisfactorily the maximum run-up, also the water surface elevation in the residual lake after the event.
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