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Potential & Challenges of Pol-InSAR Techniques  for Forest Height Estimation in the context of the BIOMASS Mission S-K. Lee, S. Sauer, F. Kugler, R. Scheiber, I. Hajnsek & K. Papathanassiou German Aerospace Center (DLR)  Microwaves and Radar Institute (DLR-HR)
Motivation 26 Plots / 27m x 32m /  l a = 0.6 Sungai Wain Lowland Dipterocarp Forest Mawas 1 Riverine Peat Swamp Forest Mawas 2 Tropical Peat Swamp Forest 20 Plots / 10m x 10m /  l a = 0.5 20 Plots / 10m x 10m /  l a = 0.6 Insufficient Number of samples !!!   -  But clear trend visible !!!
Volume Coherence …  vertical reflectivity function Interferometric  Coherence Volume  Coherence Vertical Wavenumber: G/V Ratio: Volume Height Extinction Topography G/V Ratio 2 Layer Scattering Model
The Effect of the Ground-2-Volume Component  Phase Center Location as a Function of Polarisation / Ground Variance of the Phase Center Location due to  Volume,  System and  Temporal  Decorrelation Ground and Volume  No Ground  Only Volume Volume only
Campaigns Summary Lidar 4 - 6m / .5 -.7 30º-45º Flat Multiple >2 15min Managed Semi Boreal BIOSAR-I Lidar 4.5m / .65 30º-50º Hilly Multiple >2 15min  Boreal BIOSAR-II Lidar 1.9m / .95 30°-45° Locally Slopes Multiple >2 15 min Temperate TempoSAR Stand < 2m 30°-40° Flat 1 15 min Managed Temperate Nezer Forest Lidar 2.m / .94 35º-40º Flat 3 20min Peat Swamp  INDREX-II Stands 2-3m 40º Hilly 2 20min (Lowland) Dipterocarp  INDREX-II 30-40º Incidence Angle 2,5m (Preliminary) Results RMS / ρ2 15 min + … Temporal Baseline Stand Hilly 1 Tropical TropiSAR Terrain Forest Campaign Reference Spatial Baselines
Ground-2-Volume Ratios Range INDREX-II: 1402; Mawas INDREX-II: 0601; Sungai Wain m max m min
Ground-2-Volume Ratios Range BioSAR 2007: 0401; Remningstorp m max m min BioSAR 2008: 0103; Krycklan
Model Miss-Match of Vertical Structure Function (f(z)) P-band P-band 50 40 30 20 10 0 m MAWAS Krycklan Forest Height Forest Height LIDAR H100 (m) LIDAR H100 (m)
Effect of Extinction and Ground-to-Volume Ratio σ   > 0 m 3 = 0 σ   > 0 m 3 ≠  0 σ  >< 0 m 3 = 0 σ  >< 0 m 3 ≠  0
Campaigns Summary Temporal Deco 2 Layer Model with Temporal Decorrelation Extinction Volume  Coherence Volume Height Topography G/V Ratio Temp. Deco. Volume Temp. Deco. Ground 1-7d 2 / 4 / 7 / 14 / 20 / 22d 1 - 15d 1 / 30 / 56d 20min Temporal Baseline 0.94 / 0.85 / 0.90 / 0.80 / 0.92 / 0.90 Tropical TropiSAR 0.95 - 0.95 Managed Temperate TempoSAR Tropical Managed Semi Boreal Peat Swamp  Forest La Selva BIOSAR-I INDREX-II Campaign Lidar Lidar Comments 0.6-0.8 0.95 / 0.9 / 0.85  0.93 Temporal Decorrelation 10m 20m 30m
Campaigns Summary Temporal Deco with Volume Coherence & Decorrelation 1-7d 2 / 4 / 7 / 14 / 20 / 22d 1 - 15d 1 / 30 / 56d 20min Temporal Baseline 0.94 / 0.85 / 0.90 / 0.80 / 0.92 / 0.90 Tropical TropiSAR 0.95 - 0.95 Managed Temperate TempoSAR Tropical Managed Semi Boreal Peat Swamp  Forest La Selva BIOSAR-I INDREX-II Campaign Lidar Lidar Comments 0.6-0.8 0.95 / 0.9 / 0.85  0.93 Temporal Decorrelation 10m 20m 30m
From Air 2 Space-Borne ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Decorrelation Modeling Phase Screens Phase & Amplitude Deco
Deterioration of Resolution (P-band BIOSAR) Original airborne resolution (2m x 5m Multilook) Degraded resolution (50m x 50m Multilook)
BIOSAR-I: Interferometric  Coherence History 100MHz 6MHz HH Channel 6MHz + NESZ + Ambiguities T-deco = 0.9 Coheren c e 6MHz Coheren c e 100MHz
BIOSAR-I: Interferometric  Coherence History 100MHz 6MHz HH Channel 6MHz + NESZ + Ambiguities T-deco = 0.9
Mawas Test Site / INDREX-II Remningstorp Test Site Kryckland Test Site Mawas Test Site HV Amplitude 100MHz 6MHz HV Amplitude 100MHz 6MHz HV Amplitude 100MHz 6MHz
BIOSAR-I: Single & Dual Baseline Inversion of Forest Height Single baseline inversion; Original data (100MHz) i Single baseline inversion; Spaceborne scenario (6MHz) i Single baseline inversion; Spaceborne scenario + T-deco  Dual baseline inversion; Spaceborne scenario + T-deco
P-band Pol-InSAR Conclusions  ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
P-band Pol-InSAR Conclusions  ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Potential & Challenges of Pol-InSAR Techniques  for Forest Height Estimation in the context of the BIOMASS Mission S-K. Lee, S. Sauer, F. Kugler, R. Scheiber, I. Hajnsek & K. Papathanassiou German Aerospace Center (DLR)  Microwaves and Radar Institute (DLR-HR)

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IGARSS2011-BIOMASS_Kostas_v1.ppt

  • 1. Potential & Challenges of Pol-InSAR Techniques for Forest Height Estimation in the context of the BIOMASS Mission S-K. Lee, S. Sauer, F. Kugler, R. Scheiber, I. Hajnsek & K. Papathanassiou German Aerospace Center (DLR) Microwaves and Radar Institute (DLR-HR)
  • 2. Motivation 26 Plots / 27m x 32m / l a = 0.6 Sungai Wain Lowland Dipterocarp Forest Mawas 1 Riverine Peat Swamp Forest Mawas 2 Tropical Peat Swamp Forest 20 Plots / 10m x 10m / l a = 0.5 20 Plots / 10m x 10m / l a = 0.6 Insufficient Number of samples !!! - But clear trend visible !!!
  • 3. Volume Coherence … vertical reflectivity function Interferometric Coherence Volume Coherence Vertical Wavenumber: G/V Ratio: Volume Height Extinction Topography G/V Ratio 2 Layer Scattering Model
  • 4. The Effect of the Ground-2-Volume Component Phase Center Location as a Function of Polarisation / Ground Variance of the Phase Center Location due to Volume, System and Temporal Decorrelation Ground and Volume No Ground Only Volume Volume only
  • 5. Campaigns Summary Lidar 4 - 6m / .5 -.7 30º-45º Flat Multiple >2 15min Managed Semi Boreal BIOSAR-I Lidar 4.5m / .65 30º-50º Hilly Multiple >2 15min Boreal BIOSAR-II Lidar 1.9m / .95 30°-45° Locally Slopes Multiple >2 15 min Temperate TempoSAR Stand < 2m 30°-40° Flat 1 15 min Managed Temperate Nezer Forest Lidar 2.m / .94 35º-40º Flat 3 20min Peat Swamp INDREX-II Stands 2-3m 40º Hilly 2 20min (Lowland) Dipterocarp INDREX-II 30-40º Incidence Angle 2,5m (Preliminary) Results RMS / ρ2 15 min + … Temporal Baseline Stand Hilly 1 Tropical TropiSAR Terrain Forest Campaign Reference Spatial Baselines
  • 6. Ground-2-Volume Ratios Range INDREX-II: 1402; Mawas INDREX-II: 0601; Sungai Wain m max m min
  • 7. Ground-2-Volume Ratios Range BioSAR 2007: 0401; Remningstorp m max m min BioSAR 2008: 0103; Krycklan
  • 8. Model Miss-Match of Vertical Structure Function (f(z)) P-band P-band 50 40 30 20 10 0 m MAWAS Krycklan Forest Height Forest Height LIDAR H100 (m) LIDAR H100 (m)
  • 9. Effect of Extinction and Ground-to-Volume Ratio σ > 0 m 3 = 0 σ > 0 m 3 ≠ 0 σ >< 0 m 3 = 0 σ >< 0 m 3 ≠ 0
  • 10. Campaigns Summary Temporal Deco 2 Layer Model with Temporal Decorrelation Extinction Volume Coherence Volume Height Topography G/V Ratio Temp. Deco. Volume Temp. Deco. Ground 1-7d 2 / 4 / 7 / 14 / 20 / 22d 1 - 15d 1 / 30 / 56d 20min Temporal Baseline 0.94 / 0.85 / 0.90 / 0.80 / 0.92 / 0.90 Tropical TropiSAR 0.95 - 0.95 Managed Temperate TempoSAR Tropical Managed Semi Boreal Peat Swamp Forest La Selva BIOSAR-I INDREX-II Campaign Lidar Lidar Comments 0.6-0.8 0.95 / 0.9 / 0.85 0.93 Temporal Decorrelation 10m 20m 30m
  • 11. Campaigns Summary Temporal Deco with Volume Coherence & Decorrelation 1-7d 2 / 4 / 7 / 14 / 20 / 22d 1 - 15d 1 / 30 / 56d 20min Temporal Baseline 0.94 / 0.85 / 0.90 / 0.80 / 0.92 / 0.90 Tropical TropiSAR 0.95 - 0.95 Managed Temperate TempoSAR Tropical Managed Semi Boreal Peat Swamp Forest La Selva BIOSAR-I INDREX-II Campaign Lidar Lidar Comments 0.6-0.8 0.95 / 0.9 / 0.85 0.93 Temporal Decorrelation 10m 20m 30m
  • 12.
  • 13. Decorrelation Modeling Phase Screens Phase & Amplitude Deco
  • 14. Deterioration of Resolution (P-band BIOSAR) Original airborne resolution (2m x 5m Multilook) Degraded resolution (50m x 50m Multilook)
  • 15. BIOSAR-I: Interferometric Coherence History 100MHz 6MHz HH Channel 6MHz + NESZ + Ambiguities T-deco = 0.9 Coheren c e 6MHz Coheren c e 100MHz
  • 16. BIOSAR-I: Interferometric Coherence History 100MHz 6MHz HH Channel 6MHz + NESZ + Ambiguities T-deco = 0.9
  • 17. Mawas Test Site / INDREX-II Remningstorp Test Site Kryckland Test Site Mawas Test Site HV Amplitude 100MHz 6MHz HV Amplitude 100MHz 6MHz HV Amplitude 100MHz 6MHz
  • 18. BIOSAR-I: Single & Dual Baseline Inversion of Forest Height Single baseline inversion; Original data (100MHz) i Single baseline inversion; Spaceborne scenario (6MHz) i Single baseline inversion; Spaceborne scenario + T-deco Dual baseline inversion; Spaceborne scenario + T-deco
  • 19.
  • 20.
  • 21. Potential & Challenges of Pol-InSAR Techniques for Forest Height Estimation in the context of the BIOMASS Mission S-K. Lee, S. Sauer, F. Kugler, R. Scheiber, I. Hajnsek & K. Papathanassiou German Aerospace Center (DLR) Microwaves and Radar Institute (DLR-HR)

Editor's Notes

  1. Polarimetry allows to decompose scattering processes but, do not provide sensitivity to the vertical structure of the scatterer, in other words to the vegetation volume itself. This is because of the two-dimensional imaging geometry of the SAR: ground range and height are projected onto slant range and become ambiguous. The key to the vertical structure is provided by InSAR: As many of you may know InSAR is a technique that allows the estimation of the height of the phase center and thus the generation of DEMs. It is based on the acquisition of two images from slightly different look angles. The main observable is the interferometric coherence: the complex cross-correlation of the two images. The inteferometric coherence can be decomposed into different contributions: temporal …, noise induced decorrelation, and volume decorrelation. And this last term is especially important. Why? Because it is directly related to the vertical reflectivity function of the scatterer, i.e. to its vertical stucture as seen by the radar. To illustrate better this important point lets take a slice through the vegetation layer: the scattering is maximum on the top and gets attenuated as the wave propagates through the volume layer. On the bottom you have again a strong ground contribution. I.e. it has a vertical reflectivity function as this: … The interferometric volume coherence for this slice is nothing more than the (normalised) fourier transform of f(z). Thus, interferometry provides an observation space sensitive to vertical structure.