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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’.

Hydrological investigations in the Rétköz, Hungary

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In this research the Modified Normalized Difference Water Index was used to enhance and map the open water features in a Hungarian sample area. Two Landsat-7 ETM+ images from 23. April and 30. September 2000 were used to derive the final maps. The sample area is highly endangered by excess water inundation therefore the rapid mapping of water surfaces is necessary. As result the MNDWI can be used for quick mapping, the result maps matched the distrubution of water closely. Presented by Balázs Boglárka, assistant professor at Debrecen University

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Page 1: Hydrological investigations in the Rétköz, Hungary

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’.

Page 2: Hydrological investigations in the Rétköz, Hungary

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

Page 3: Hydrological investigations in the Rétköz, Hungary

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 ?!

Page 4: Hydrological investigations in the Rétköz, Hungary

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

Page 5: Hydrological investigations in the Rétköz, Hungary

Sample area

275 km2

Page 6: Hydrological investigations in the Rétköz, Hungary

Sample area

Page 7: Hydrological investigations in the Rétköz, Hungary

Sample area

Page 8: Hydrological investigations in the Rétköz, Hungary

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

+

Page 9: Hydrological investigations in the Rétköz, Hungary

Resultso Satellite image covered 94.3% of the sample areao 10.9 km2 water surface and saturated surfaceo 4% of the whole Rétköz

Page 10: Hydrological investigations in the Rétköz, Hungary

Results

Page 11: Hydrological investigations in the Rétköz, Hungary

Results

Page 12: Hydrological investigations in the Rétköz, Hungary

Results

Threshold: 0

Page 13: Hydrological investigations in the Rétköz, Hungary

Results

NDVI values

Page 14: Hydrological investigations in the Rétköz, Hungary

Results

Threshold: 0.15

Water: 1.24 km2,0.45% of Rétköz

Page 15: Hydrological investigations in the Rétköz, Hungary

Thank you for your attention!

[email protected]

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