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A land cover map of Africa at 100m using a mosaic of ALOS PALSAR  dual-polarization data   - Preliminary developments - Alexandre Bouvet, Gianfranco De Grandi European Commission DG Joint Research Centre 21027, Ispra (VA), Italy e-mail:  [email_address]
ALOS Kyoto & Carbon (K&C) Initiative CONTEXT Global coverage of the African continent with PALSAR observations at two polarizations (HH + HV), one date (mainly July-August 2007) Objectives of K&C: define, develop and validate thematic products used to meet the specific information requirements relating to the  international environmental Conventions, Carbon Cycle Science and Conservation of the environment Systematic data acquisition strategy ,[object Object],[object Object],De Grandi et al., IEEE TGRS, in press
VCF  (Vegetation Continuous Field) University of Maryland - NASA MODIS - 500m GLC2000 (Global Land Cover 2000) JRC SPOT VEGETATION - 1km   GLOBCOVER ESA - JRC MERIS – 300m EXISTING LARGE-SCALE MAPS
VCF GLC2000 GLOBCOVER PALSAR HV ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],PRELIMINARY APPROACH
East North incident wave     lon lat INFLUENCE OF TOPOGRAPHY Local incidence angle: θ loc  depends on: θ : the SAR incident angle φ : the viewing azimuth angle α : the absolute slope β : the slope orientation In the mosaic, the SAR geometry is almost constant: θ≈ 39˚  φ≈ 10.5˚  θ loc  is fully described by the local topography ( α  and  β ). SAR geometry local topography
correction of effective scattering area  correction of backscatter angular dependence  (exact correction) (approximated correction – dependant on land cover type) INFLUENCE OF TOPOGRAPHY ,[object Object],[object Object],[object Object]
Detail Not corrected TOPOGRAPHIC CORRECTION
INFLUENCE OF TOPOGRAPHY Tropical forest sin sin & cos
INFLUENCE OF TOPOGRAPHY Shrubland sin sin & cos
INFLUENCE OF TOPOGRAPHY Tropical forest facing perpendicular opposite sin sin & cos
INFLUENCE OF TOPOGRAPHY Shrubland facing perpendicular opposite sin sin & cos
INFLUENCE OF TOPOGRAPHY ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
S01 E09 (Gabon) 1990 2000 ,[object Object],[object Object],[object Object],[object Object],[object Object],CLASSIFICATION
BACKSCATTER SIGNATURES Tropical forest
BACKSCATTER SIGNATURES Shrubland
S01 E09 (Gabon) 1990 2000 ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],CLASSIFICATION
WATER BODIES HH-HV-HH White:  α =0° Grey: buffer 10 pix Classified Pros: false detection (bare soil/low vegetation detected as water) is reduced Cons: some water bodies are missed
VCF GLC Tile centered on:  32.5°S–27.5° E South Africa RESULTS VCF GLC2000 GLOBCOVER PALSAR
Tile centered on: 2.5°S – 17.5° E Border between the Congos Transition from tropical forest to savanna. VCF GLC GlobCover VCF GLC2000 GLOBCOVER PALSAR RESULTS
PALSAR GlobCover 2009 Central African tile Subset 1 RESULTS
Central African tile Subset 2 RESULTS PALSAR GlobCover
PALSAR GlobCover South African tile Subset 1 RESULTS PALSAR GlobCover
Reference data from the Global Forest Resources Assessment 2010 (FRA2010) Remote Sensing Survey (RSS) – FAO & JRC ,[object Object],[object Object],[object Object],1990 2000 VALIDATION Tree cover Tree cover mosaic Shrub Other vegetation Water
2°S – 16° E 1990 2000 VALIDATION
VALIDATION erosion Confusion matrices ,[object Object],[object Object],[object Object],[object Object],Pixel-based accuracies: Not eroded Eroded Land cover 72.4% 79.4% Forest/non-forest 88.3% 93.9%
[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],CONCLUSION & PERSPECTIVES

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Bouvet_IGARSS2011.ppt

  • 1. A land cover map of Africa at 100m using a mosaic of ALOS PALSAR dual-polarization data - Preliminary developments - Alexandre Bouvet, Gianfranco De Grandi European Commission DG Joint Research Centre 21027, Ispra (VA), Italy e-mail: [email_address]
  • 2.
  • 3. VCF (Vegetation Continuous Field) University of Maryland - NASA MODIS - 500m GLC2000 (Global Land Cover 2000) JRC SPOT VEGETATION - 1km GLOBCOVER ESA - JRC MERIS – 300m EXISTING LARGE-SCALE MAPS
  • 4.
  • 5. East North incident wave     lon lat INFLUENCE OF TOPOGRAPHY Local incidence angle: θ loc depends on: θ : the SAR incident angle φ : the viewing azimuth angle α : the absolute slope β : the slope orientation In the mosaic, the SAR geometry is almost constant: θ≈ 39˚ φ≈ 10.5˚ θ loc is fully described by the local topography ( α and β ). SAR geometry local topography
  • 6.
  • 7. Detail Not corrected TOPOGRAPHIC CORRECTION
  • 8. INFLUENCE OF TOPOGRAPHY Tropical forest sin sin & cos
  • 9. INFLUENCE OF TOPOGRAPHY Shrubland sin sin & cos
  • 10. INFLUENCE OF TOPOGRAPHY Tropical forest facing perpendicular opposite sin sin & cos
  • 11. INFLUENCE OF TOPOGRAPHY Shrubland facing perpendicular opposite sin sin & cos
  • 12.
  • 13.
  • 16.
  • 17. WATER BODIES HH-HV-HH White: α =0° Grey: buffer 10 pix Classified Pros: false detection (bare soil/low vegetation detected as water) is reduced Cons: some water bodies are missed
  • 18. VCF GLC Tile centered on: 32.5°S–27.5° E South Africa RESULTS VCF GLC2000 GLOBCOVER PALSAR
  • 19. Tile centered on: 2.5°S – 17.5° E Border between the Congos Transition from tropical forest to savanna. VCF GLC GlobCover VCF GLC2000 GLOBCOVER PALSAR RESULTS
  • 20. PALSAR GlobCover 2009 Central African tile Subset 1 RESULTS
  • 21. Central African tile Subset 2 RESULTS PALSAR GlobCover
  • 22. PALSAR GlobCover South African tile Subset 1 RESULTS PALSAR GlobCover
  • 23.
  • 24. 2°S – 16° E 1990 2000 VALIDATION
  • 25.
  • 26.