- The steps for geocoding, for a complex case 
with LANDSAT and SAR-ERS recordings, are: 
= the visualisation of the CCT or other remote 
sensing recordings; 
= the digitising of the contour lines; 
= selection of GCP (ground control points) for 
LANDSAT and SAR-ERS simulated 
images and the registration-fusion of them 
with DTM creation(Schreier 1993). 
- The  registration-fusion between the 
LANDSAT and SAR-ERS-PRI geocoded. 
- 3D perspectives of the geocoded images(see 
slides 1-9). 
- Marine driling profiles and their afferent 
classical determinations positioning an the 
aerial satelite recordings. 
-  Radiometric seasonal profiles built on 
characteristic and — suggesstive directions, 
basicaly on the “Great Deltaic Profile”; and on 
different ecosystems (see fig.2); 
  
Figure 2. The Great Deltaic Profile 
- Preliminary processing of SAR-ERS 
recordings, taken as reference level: 
= recording segmentation; 
" on ecosystems bases; 
* on hydrographic basins and microbasins 
bases; 
= visualisation, with succesive adjustments 
using PDF (Probability Density Function); 
= speckle attenuations using adaptive and 
geometric filters; 
= colour — composed RGB and [HS system 
processings, as well as transformations from 
RGB to IHS, on the whole recording (or 
wide areas), on image segmentations 
respectively. 
- Preliminary processings of the satellite 
recordings in optical domain: 
= the edges enhancement on the thematic 
contrast enhancement on spectral bands 
combinations and also on radio of i, j, 
bands; 
= edge detection with convolution kernels: 
Sobel, Prewitt, (Pratt 1991) (fig.4). 
4. IMAGE PROCESSING AND OBTAINED 
RESULTS. 
- Improvement of the drawing of the areas 
with microrelief zones, using radar recordings 
on the dry-normal periods. 
- Monitoring — control of the “red 
blossoming” — biological pollution in the 
coastal area of the Black Sea between Niepre 
Lagoon and Boshphorus (cca. 650km see fig.3). 
- Monitoring of the oil slices type pollution 
on the sea especially in area of driling 
platforms. 
- Monitoring of the morphological evolution 
of the coastal regime, especially on the Sachalin 
Island in the period 1972 - 1993. 
- The sediments discharge in the Black Sea, 
on the Danube mouths and the coastal zone of 
the Black Sea (see fig.3). 
  
Figure 3. Biological pollution and sediments 
discharge in the coastal zone of the 
Black Sea. 
  
  
  
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