Table 3 Computed flow depth and flow velocity at the position of boulders by the waves
From: Numerical simulations to account for boulder movements on Lanyu Island, Taiwan: tsunami or storm?
ID | 19-year return period | 50-year return period | 100-year return period | |||
|---|---|---|---|---|---|---|
Flow depth (m) | Flow velocity (m/s) | Flow depth (m) | Flow velocity (m/s) | Flow depth (m) | Flow velocity (m/s) | |
1 | 0.5 | 1.1 | 2.1 | 2.3 | 3.1 | 9.7 |
2 | 0.6 | 1.2 | 1.9 | 5.9 | 3.2 | 10.3 |
3 | 0.7 | 1.3 | 1.9 | 6.0 | 3.3 | 10.6 |
4 | 2.3 | 5.3 | 3.8 | 8.0 | 6.8 | 12.7 |
5 | 2.5 | 5.3 | 3.8 | 7.7 | 5.9 | 12.2 |
6 | 2.4 | 5.3 | 3.8 | 7.9 | 6.1 | 12.3 |
7 | 2.5 | 6.1 | 5.6 | 7.9 | 7.6 | 13.1 |
8 | 2.4 | 6.1 | 5.6 | 7.8 | 7.6 | 13.0 |
9 | 2.7 | 6.2 | 6.4 | 8.0 | 7.5 | 13.4 |
10 | 5.1 | 7.4 | 5.9 | 9.4 | 9.2 | 13.7 |
11 | 3.0 | 6.1 | 6.7 | 7.9 | 7.7 | 13.4 |
12 | 4.1 | 7.2 | 5.4 | 9.6 | 6.4 | 11.0 |
13 | 4.8 | 9.6 | 5.4 | 12.2 | 7.0 | 12.7 |
14 | 5.3 | 8.9 | 5.9 | 12.1 | 5.9 | 12.8 |
15 | 2.3 | 5.5 | 3.3 | 7.9 | 5.7 | 9.5 |
16 | 2.6 | 6.3 | 5.0 | 8.8 | 6.3 | 10.1 |
17 | 4.0 | 8.2 | 4.7 | 9.9 | 6.8 | 10.7 |
18 | 4.5 | 7.5 | 5.4 | 9.4 | 6.1 | 10.1 |
19 | 1.3 | 4.9 | 2.4 | 7.0 | 4.5 | 8.3 |
20 | 1.3 | 4.4 | 2.2 | 6.9 | 3.3 | 8.2 |
21 | 1.3 | 4.5 | 2.3 | 6.9 | 3.4 | 8.1 |
22 | 5.9 | 9.9 | 9.4 | 11.5 | 10.0 | 12.3 |
23 | 4.4 | 9.3 | 8.1 | 10.8 | 9.3 | 11.8 |
24 | 3.1 | 7.1 | 6.7 | 9.5 | 6.8 | 10.8 |
25 | 5.7 | 10.1 | 6.4 | 12.0 | 8.3 | 12.6 |
26 | 5.3 | 10.1 | 6.7 | 11.5 | 8.2 | 12.6 |
27 | 5.5 | 10.3 | 7.3 | 11.9 | 8.3 | 12.9 |
28 | 4.7 | 8.0 | 5.2 | 9.8 | 6.1 | 11.5 |
29 | 3.1 | 7.1 | 6.8 | 9.5 | 6.8 | 10.8 |
30 | 5.1 | 8.5 | 6.4 | 10.0 | 9.3 | 13.2 |
31 | 0.5 | 0.8 | 1.1 | 2.0 | 2.9 | 5.3 |
32 | 0.5 | 0.8 | 1.1 | 2.0 | 2.9 | 5.3 |
33 | 0.2 | 0.2 | 1.0 | 1.6 | 3.0 | 5.0 |
34 | 0.5 | 0.7 | 1.1 | 1.9 | 2.9 | 5.2 |