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Hydrological Investigations in
The Rétköz, Hungary
Boglárka Balázs ‒ Gábor Türk
29-31 May, 2014 Hungarian GIS Conference with MapWindow
This research was supported by the European Union
and the State of Hungary, co-financed by the European Social Fund in
the framework of TÁMOP 4.2.4.A/2-11-1-2012-0001 ‘National
Excellence Program’.
Intro ─ Remote Sensing in Mapping Surface Water
 Different materials reflect differently at different
wavelenghts
 Widely used for surface analysing
 Opportunity to map surface water
 Monitor the dynamics of surface water
 Different methods to extract water features:
 Single-band method – threshold?  under/over-
estimation
 Multi-band methods (reflective differences between
bands)
 If-then-else logic tree (analysing signature among different
spectral bands, find differences, then use the tree)
 Band-ratio approach – spectral indexes
Intro ─ Spectral indexes
 Single number derived from an arithmetic operation
 NDVI = (NIR−Red)/(NIR+Red)
 NDWI McFeeters = (Green−NIR)/(Green+NIR)  -1 ≤ NDWI ≤ 1
Threshold: 0
 NDWI Gao= (NIR−SWIR)/(NIR+SWIR) water content of vegetation
canopy
 MNDWI= (Green−SWIR)/(Green+SWIR)
Threshold: 0, but more accurate results can be achieved by manual
adjustment
 Threshold ?!
Why could the NDWI be so important in Hungary?
 More than half is flatland
 Inundation hazard map of Hungary by Pálfai, I. (2003)
 60% of the flatland is differently endangered by inundation
 5% highly endangered
 26% medium risk
 29% low risk
 40% barely endangered
Sample area
275 km2
Sample area
Sample area
Satellite images
 Landsat-7 ETM+ images
 23. April 2000
 30. September 2000
 Seasons with different aspect
MNDWI= (B2−B5)/(B2+B5)
Water ≥0; non-water ≤0
−
+
Results
o Satellite image covered 94.3% of the sample area
o 10.9 km2 water surface and saturated surface
o 4% of the whole Rétköz
Results
Results
Results
Threshold: 0
Results
NDVI values
Results
Threshold: 0.15
Water: 1.24 km2,
0.45% of Rétköz
Thank you for your
attention!
geo.bb@mailbox.hu
?

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Hydrological investigations in the Rétköz, Hungary

  • 1. Hydrological Investigations in The Rétköz, Hungary Boglárka Balázs ‒ Gábor Türk 29-31 May, 2014 Hungarian GIS Conference with MapWindow This research was supported by the European Union and the State of Hungary, co-financed by the European Social Fund in the framework of TÁMOP 4.2.4.A/2-11-1-2012-0001 ‘National Excellence Program’.
  • 2. Intro ─ Remote Sensing in Mapping Surface Water  Different materials reflect differently at different wavelenghts  Widely used for surface analysing  Opportunity to map surface water  Monitor the dynamics of surface water  Different methods to extract water features:  Single-band method – threshold?  under/over- estimation  Multi-band methods (reflective differences between bands)  If-then-else logic tree (analysing signature among different spectral bands, find differences, then use the tree)  Band-ratio approach – spectral indexes
  • 3. Intro ─ Spectral indexes  Single number derived from an arithmetic operation  NDVI = (NIR−Red)/(NIR+Red)  NDWI McFeeters = (Green−NIR)/(Green+NIR)  -1 ≤ NDWI ≤ 1 Threshold: 0  NDWI Gao= (NIR−SWIR)/(NIR+SWIR) water content of vegetation canopy  MNDWI= (Green−SWIR)/(Green+SWIR) Threshold: 0, but more accurate results can be achieved by manual adjustment  Threshold ?!
  • 4. Why could the NDWI be so important in Hungary?  More than half is flatland  Inundation hazard map of Hungary by Pálfai, I. (2003)  60% of the flatland is differently endangered by inundation  5% highly endangered  26% medium risk  29% low risk  40% barely endangered
  • 8. Satellite images  Landsat-7 ETM+ images  23. April 2000  30. September 2000  Seasons with different aspect MNDWI= (B2−B5)/(B2+B5) Water ≥0; non-water ≤0 − +
  • 9. Results o Satellite image covered 94.3% of the sample area o 10.9 km2 water surface and saturated surface o 4% of the whole Rétköz
  • 14. Results Threshold: 0.15 Water: 1.24 km2, 0.45% of Rétköz
  • 15. Thank you for your attention! geo.bb@mailbox.hu ?