at December 25, 1996. In this imagery, we easily interpreted by
visually for land use land cover condition of Yangon river in
and around and City area.
b es ants
"ns
Lanisat 132 Color Composite Ortborectifüsd Impe
Acquisiiun Date: Feb 25, 2006
Map Sci: t0 0
Figure 5. Landsat 432 Color Composite Ortho-rectified Image
acquisition at Feb 25,2006
In Figure 5, Landsat Satellite acquired with ETM-- Sensor for
the study area. After composite of FCC 432 combination was
done and carefully analyzed for landuse landcover extended
and urban, sub-urban sprawled areas.
Laanhat 332 FIC Oni horostifecd Teray:
Aóguisitkots dote: Me S, O00
Mage Scde 11808
Figure 6. Landsat 432 Color Composite Ortho-rectified Image
acquisition at March 3,2009
International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences, Volume XXXIX-B8, 2012
XXII ISPRS Congress, 25 August — 01 September 2012, Melbourne, Australia
In May 2 of 2008, Myanmar was seriously hit by Cyclone
Nargis and there was damaged to coastal mangrove areas and
its biodiversity system in and around of Yangon river terraces
(see figure 6).
4.2 Interpretation and terrain analysis from RADAR data
Figure 7. JERS 1 SAR Multi Temporal image of study area
In Figure 7, Japan Earth Observation Satellite was taken
Synthetic Aperture Radar (SAR) imagery for 3 different
seasons of around 1996. Coastal surveillance and
environmental monitoring has motivated the development of
automatized feature extraction tools using remote sensing data.
Target detection by Synthetic Aperture Radar (SAR) has been
extensively studied in recent years. In carefully interpretation
from SAR Imagery, river boundary and coast line field give
high radar backscattered energy due to their high surface for
roughness. Strong waves and tides (surfing in particular) make
seawater very rough which leads to very high radar
backscattered energy at places. Coastline is therefore masked at
places between land and water boundary.
Figure 8. SRTM data of Yangon river rings
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