A Robust System for Shoreline Detection and its Application to Coastal-zone Monitoring
Test Data and Results
Figure 3.1 is a SPOT multi-spectral image acquired on Nov. 12, 1998. It is a shelf near
western coast of Taiwan. The red line is detected shoreline by proposed scheme. The yellow
line is a ground survey result using DGPS(Differential Global Positioning System) at the same
time with the accuracy under one meter. The error checking positions are indicated as green
segments. Table 3.1 is the error of each segment.

Figure 3.1 Test SPOT images.
|
Table 3.1 Error of each segment.
| Segment No. | Absolute Length(m) |
| 1 | 20 |
| 2 | 22 |
| 3 | 19 |
| 4 | 14 |
| 5 | 32 |
| 6 | 15 |
| 7 | 13 |
| 8 | 16 |
| 9 | 19 |
| 10 | 26 |
| 11 | 13 |
| 12 | 16 |
| 13 | 14 |
| 14 | 15 |
| 15 | 18 |
|
From table 3.1, the error is around one image pixel. This result illustrates the
practicability of proposed scheme. In figure 3.2, a series of SPOT images acquired
during Nov. 1 and Nov. 12, 1998. The location of these images is the southern coast of
Taichung Harbor. In this period, the sea level varies from 85.8cm to 515.6cm. Figure
3.3 shows the detected shorelines and demonstrates the contours of tideland.
 |
11/03/1998, 515.6cm
| 11/02/1998, 451.3cm | 11/01/1998, 339.3cm |
 | |
11/12/1998, 125.8cm
| 11/11/1998, 85.8cm |
Figure 3.2 A series of test SPOT images and their sea levels.

Figure 3.3 The detected shorelines of tideland.
Figure 3.4 is two SPOT images at a time interval of 5 years over Taichung
Harbor. Their sea levels are 122.7cm and 125.8cm, respectively. Figure 3.5
demonstrates the time variation of the tideland over the same area.
 |
12/08/1993, 122.7cm
|
11/12/1998, 125.8cm |
Figure 3.4 Two SPOT images at a time interval of 5 years and their sea levels.
|

Figure 3.5 The time variation of the tideland over the same area.
Conclusion
From the comparison of detected shoreline and ground survey, the results
illustrate the proposed scheme is capable of detecting shoreline automatically.
Obviously, if a series of images within a short period of time can be collected,
we can delineate contours of the tideland. Accordingly, if a series of images with their
time interval is long enough and the sea levels are similar, we can detect the variation
of tideland. From the result of the test data shows that the tideland of the southern
coast of Taichung Harbor is shrinking.
Reference
- Conrac Corp., “Raster Graphics Handbook”, Conrac Division, 1980.
- Rafael C. Gonzalez and Richard E. Woods, “Digital Image Processing”,
Addsion-Wesely, 1992.