Summary Modul CMS

1. IntroductionCMS digunakan untuk memodelkan gelombang, tinggi muka air, transpor sedimen, dan perubahan morfologi pantai.

Figure 1. CMS flowchart

Figure 2. Mean values of Nikradse roughness heights for different bottom types

Figure 3. Base Mannings n coefficients as a function of the median grain size for the upper flow regime (Benson and Dalrymple 1984).

Figure 4 Wave transmision and overtoping at strucutre