International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences, Vol XXXV, Part B7. Istanbul 2004
limited. And the flood water depth or the necessary
information on regional base is not easily acquired by the
remote sensing data. Then it should be very convenient that the
above mentioned information can be uploaded into the web
servers which exist at hand, but the client of disaster
information unconsciously and seamlessly can access such
kind data on the distributed and cooperated web servers
through the Internet. Recently, the discussion of the
international standard for such distributed and cooperated
server design is progressing at ISO, OGC, etc.
Mathematical morphology procedure should be suitable
for the method of SAR data analysis for such kind of disaster
data server. Because this image processing procedure will
have advantage over the flood disaster monitoring using SAR
satellite data in some points.
The authors plan to make rapidly flood extent mapping
server on the Internet for the early warning system of regional
and agricultural flood damage.
2. FLOOD EXTENT MAPPING METHOD IN
HI dilation dilation
— —
erosion erosion
—- —
Fig.1 The results of dilation and erosion
22 Terrain feature recognition method for SAR imagery
in paddy field areas during flood
If the farm lane or levee is above the water surface
otherwise it is an ordinary inundation or flood, the flood
PADDY FIELD AREAS
2.1 Interaction between SAR data and ground features
Computational mathematical morphology operations,
such as erosion, dilation, opening, closing and directional
filters, provide image feature measurements. By using
conventional method, they can detect the flood extent from the
low backscattering value of each pixel for the water surface.
But it will be very difficult to distinguish the flood areas from
the ordinary paddy fields especially in the early growing stage
of rice plants. But SAR signal intensity for each pixel
includes some interactive information between microwave and
terrain feature on the ground. Then morphological processing
procedures are one of the methods for detecting such spatial
information. For example, if the Levee of paddy fields is
above the inundated water surface, the paddy fields should be
almost without damages in the consolidated farm lands. If the
region of the low backscattering intensity level occupy large
area, that can be most likely large water surface,
flood-inundated areas. These calculations require only a
snapshot of SAR image.
"Morphological operators
S#B= {z: B+z#S} ; erosion operation
S @ B=#{B+x:x#S} ; dilation operation
S $ B = (S # B) @ B ; opening operation
S Y B = [ S @ (-B)] # (-B) ; closing operation
damage to paddy rice is assumed as no damage. Because
usually, paddy fields have the water surface of its swamp and
the water level is under the top of the levee or farm lane.
rice crop
water lebel
an inundated paddy field lot
Fig2 Cross section of paddy fields
602
Internati
water su
threshok
some dil
areas of
fields.
width of
field has
run alon;
e
Th
be most
method
surface.
3.1 The
for SAR
The
"opening
followed
operatior
used to