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IGARSS 2011 	International Geosience and Remote Sensing Symposium MODELLING COASTAL PROCESSES BY MEANS OF INNOVATIVE INTEGRATION OF REMOTE SENSING TIME SERIES ANALYSIS Taramelli A.1, Valentini E.1, Dejana M.1, Zucca F.2, Mandrone S.1 1ISPRA –InstituteforEnvironmentalProtection and Research Rome– Italy 2Universita degli Studi di Pavia
OUTLINE OF THE PRESENTATION ,[object Object]
multiscale  approach;
 in situ data for remote data characterization;
 satellite imagery data fusion;
 results.,[object Object]
MODELLING Biochemistry LANDSCAPE SEASCAPE COASTAL PROXY INDEX
Feedback from geomorphological and sedimentology indicators Biological indicators selection and quantification within habitats  (both emerged and submerged) Upscaling Land/sea form system pattern Habitat selection: landscape scale definition Downscal  i ng Multisensor data collection (Satellite and field survey)  Selection of nearshore extent in each area of interest
Scientific Hypotesis i) Reflectance signature and biophysical parameters are related to each other via morphology ii) Morphological and SAR data are able to enhance hyperspectral interpretation III) Integration of different methods (Spectral Mixture Analysis, Change Detection and SBAS) to process SAR,  hyperspectral and in situ data in two different ecosystems enhance our ability to detect coastal trend
Data Sources: CAT1 Proposal C1P.7963 LANDSAT, CHRIS PROBA, ASTER  SAR, LiDAR IN SITU (vegetation pattern distribution and morphological parameters)
Studysites South Po delta and foce Bevano (Ravenna), Italy Plymouth and Erme  saltmarsh, UK Erme saltmarsh Foce Bevano
Methodology 1) Change detection NDVI analisystohighlightinter-annualchangeofvegetation 2) Change detection fractionsmapanalisysto integrate inter and intra-annualchange detection mapsofvegetationusing SMA (Small, 2001; Taramelli and Melelli, 2009) 3) Interferometric Low resolution SBAS Approach(Berardinoet al., 2002)to produce deformation and spatiotemporalvariationsmaps and Lidar morphometricanalisys(Taramelliet al., 2010) 4) Fieldvalidation and data integrationfortimeseriesanalisys
CHANGE DETECTION ANALYSIS: Po delta and Wetlands of Comacchio valley calculated NDVI  Δ image  NDVI image data 2001-08-26, path 192 row 29 NDVI (2001) – NDVI (1991) Landsat 7 ETM+ data 2001-08-26 path 192 row 29 No change Loss Gain change detection NDVI from 1991 up to 2010 with a focus on twodecades 1991-2001 and 2001-2010
METHODOLOGY SMA Endmemberscollection SpectralMixtureAnalysis classifies individual mixed pixels according to the distribution of spectrally pure end member fractions and provides a tool for discrimination and classification of surface topography. Spectral characteristics of the surface topography show significant differences between the spectral reflectance of different land-form surfaces.  A mixing space can be thought of as a coordinate system in which reflectance spectra are represented as linear mixtures of spectrally pure endmember spectra Water Wet  Soil Vegetation
Pincipal Component Analysis PCA ENDMEMBER COLLECTION
Unmixing with three pure endmebers Hyperspectralendmembers fractions map Red: anthropic/sand Green: vegetation Yellow: substrate/soil SpectralMixtureAnalysis (SMA) classifies individual mixed pixels according to the distribution of spectrally pure end member fractions. R: antropic/sand G: vegetation B: substrate/soil
In Situ vegetation and morphometric field validation  A B N
METHODOLOGY SBAS Use of a large number of radar images to reduce the various noise components of DInSARinterferograms:- maximum temporal and orbital separations are defined between the    images of each DInSARinterferogram ,[object Object]
 reference pixel is chosen by the operator
 displacement maps of each interferogram are combined together using the SVD technique to estimate ground displacement at each image date, filtering at the same time the short term atmospheric contribution,[object Object]
DataAssimilation NDVI change analysis;  mean ground velocity map vegetation fraction change analysis using fraction map.

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Taramelli_al_IGARSS_2011.pptx

  • 1. IGARSS 2011 International Geosience and Remote Sensing Symposium MODELLING COASTAL PROCESSES BY MEANS OF INNOVATIVE INTEGRATION OF REMOTE SENSING TIME SERIES ANALYSIS Taramelli A.1, Valentini E.1, Dejana M.1, Zucca F.2, Mandrone S.1 1ISPRA –InstituteforEnvironmentalProtection and Research Rome– Italy 2Universita degli Studi di Pavia
  • 2.
  • 4. in situ data for remote data characterization;
  • 5. satellite imagery data fusion;
  • 6.
  • 7. MODELLING Biochemistry LANDSCAPE SEASCAPE COASTAL PROXY INDEX
  • 8. Feedback from geomorphological and sedimentology indicators Biological indicators selection and quantification within habitats (both emerged and submerged) Upscaling Land/sea form system pattern Habitat selection: landscape scale definition Downscal i ng Multisensor data collection (Satellite and field survey) Selection of nearshore extent in each area of interest
  • 9. Scientific Hypotesis i) Reflectance signature and biophysical parameters are related to each other via morphology ii) Morphological and SAR data are able to enhance hyperspectral interpretation III) Integration of different methods (Spectral Mixture Analysis, Change Detection and SBAS) to process SAR, hyperspectral and in situ data in two different ecosystems enhance our ability to detect coastal trend
  • 10. Data Sources: CAT1 Proposal C1P.7963 LANDSAT, CHRIS PROBA, ASTER SAR, LiDAR IN SITU (vegetation pattern distribution and morphological parameters)
  • 11. Studysites South Po delta and foce Bevano (Ravenna), Italy Plymouth and Erme saltmarsh, UK Erme saltmarsh Foce Bevano
  • 12. Methodology 1) Change detection NDVI analisystohighlightinter-annualchangeofvegetation 2) Change detection fractionsmapanalisysto integrate inter and intra-annualchange detection mapsofvegetationusing SMA (Small, 2001; Taramelli and Melelli, 2009) 3) Interferometric Low resolution SBAS Approach(Berardinoet al., 2002)to produce deformation and spatiotemporalvariationsmaps and Lidar morphometricanalisys(Taramelliet al., 2010) 4) Fieldvalidation and data integrationfortimeseriesanalisys
  • 13. CHANGE DETECTION ANALYSIS: Po delta and Wetlands of Comacchio valley calculated NDVI Δ image NDVI image data 2001-08-26, path 192 row 29 NDVI (2001) – NDVI (1991) Landsat 7 ETM+ data 2001-08-26 path 192 row 29 No change Loss Gain change detection NDVI from 1991 up to 2010 with a focus on twodecades 1991-2001 and 2001-2010
  • 14. METHODOLOGY SMA Endmemberscollection SpectralMixtureAnalysis classifies individual mixed pixels according to the distribution of spectrally pure end member fractions and provides a tool for discrimination and classification of surface topography. Spectral characteristics of the surface topography show significant differences between the spectral reflectance of different land-form surfaces. A mixing space can be thought of as a coordinate system in which reflectance spectra are represented as linear mixtures of spectrally pure endmember spectra Water Wet Soil Vegetation
  • 15. Pincipal Component Analysis PCA ENDMEMBER COLLECTION
  • 16. Unmixing with three pure endmebers Hyperspectralendmembers fractions map Red: anthropic/sand Green: vegetation Yellow: substrate/soil SpectralMixtureAnalysis (SMA) classifies individual mixed pixels according to the distribution of spectrally pure end member fractions. R: antropic/sand G: vegetation B: substrate/soil
  • 17. In Situ vegetation and morphometric field validation A B N
  • 18.
  • 19. reference pixel is chosen by the operator
  • 20.
  • 21. DataAssimilation NDVI change analysis; mean ground velocity map vegetation fraction change analysis using fraction map.
  • 22. Results Gain (green) No change (white) Loss (red) Statistics within the difference image of the fraction maps and within the difference image of the NDVI Ground in central and upper part moved away from satellite with rates up to 10 cm/y Taramelli A., Valentini E., Dejana M., Zucca F., Mandrone S., 2011, MODELLING COASTAL PROCESSES BY MEANS OF INNOVATIVE INTEGRATION OF REMOTE SENSING TIME SERIES ANALYSIS, IGARSS 2011 International Geosience and Remote Sensing Symposium.
  • 23.
  • 24.