International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences, Vol XXXV, Part B2. Istanbul 2004 Intei
4. APPLICATION OF 3D VISUALIZATION OF | Figu
SEDIMENT DISASTAR Figu
| phot
4.1 Heavy Rainfall Disaster in the Kyushu District in pasti
Japan | view
Between two days from 19 to 20 in July 2002, a heavy rainfall |
attacked Kyushu district in Japan, which had caused many
kinds of disasters in various areas (Ushiyama, 2004). Especially, |
a sediment disaster in Minamata City, Kumamoto prefecture, The
was largest in this season, and 19 civilians were dead due to this Mr.
disaster. Basically, occurrences of a sediment disaster in Rese
mountain areas depend on not only soil state, but also 3 Scie
dimensional structures of land slopes. In this study, 3D
visualization of landform, where the sediment disaster occurred,
is created using 10m DEM and aerial photos.
Ushi
4.2 Integration of 10m DEM and Aerial Photos in th
138 gi. 3 Soi m ; Soci
A 1/25000 digital map by GSJ is adopted as reference data for
Minamata City area. A precise digital map in local areas is not Hokl
so popular such as ones in large cities, so a standard 1/25000
digital map is used. 10m DEM including Minamata City is
integrated with the reference data, which is shown in Figure 6.
The aerial photo, taken on 22 in July. is shown in Figure 7, at
which point the sediment disaster has occurred.
Figure 4. IKONOS colour image
©Space Imaging Co. 2002
An affine transformation is performed for integration of
IKONOS image with a digital map. There are several problems
in combining a raster image and a vector image. Especially, it is
difficult to select GCP in vector images correctly, because the
images are symbolized, and elements in a digital map are not
corresponding to a satellite image in pixel level (one-meter
resolution). On the other hand, it is easy to select GCP in
satellite images. Then, we have chosen central lines of roads as
feature layer in GIS. We show a sample for selecting GCP in
each image, using snapping effect. Thus, GCP for
transformation are selected for 30 points over the image,
equivalently. After several trials, the RMS error of 30 GCP is
finally reduced to less than one pixel, which are comparatively
good. The result of integration of IKONOS images with a
digital map is shown as in Figure 5.
Figure 5. 3D view of IKONOS image
©Space Imaging Co. 2002
Figure 7. Aerial photo at occurrence of the sediment disaster
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